wikipedia_id stringlengths 2 8 | wikipedia_title stringlengths 1 243 | url stringlengths 44 370 | contents stringlengths 53 2.22k | id int64 0 6.14M |
|---|---|---|---|---|
1402490 | Arrival and Departure | https://en.wikipedia.org/w/index.php?title=Arrival%20and%20Departure | Arrival and Departure
most shocking descriptions of Nazi terrorism that have ever been written."
# Plot.
Written during the middle of World War II, "Arrival and Departure" reflects Koestler's own plight as a Hungarian refugee. Like Koestler, the main character is a former member of the Communist party. He escapes to 'Neutralia', a neutral country based on Portugal, where Koestler himself had gone, and flees from there. (Stephen Spender had supposedly said of Neutralia, "Names like that should not be allowed in novels!") Reflecting Koestler's later life relationship with science, and particularly his disagreement with various movements within psychiatry, the main character emerges from treatment psychically neutered, | 17,500 |
1402490 | Arrival and Departure | https://en.wikipedia.org/w/index.php?title=Arrival%20and%20Departure | Arrival and Departure
arture" reflects Koestler's own plight as a Hungarian refugee. Like Koestler, the main character is a former member of the Communist party. He escapes to 'Neutralia', a neutral country based on Portugal, where Koestler himself had gone, and flees from there. (Stephen Spender had supposedly said of Neutralia, "Names like that should not be allowed in novels!") Reflecting Koestler's later life relationship with science, and particularly his disagreement with various movements within psychiatry, the main character emerges from treatment psychically neutered, and the critical question of the novel is how much of his later trauma and political activity is due to a small incident in his childhood. | 17,501 |
1402476 | George Boardman (missionary) | https://en.wikipedia.org/w/index.php?title=George%20Boardman%20(missionary) | George Boardman (missionary)
George Boardman (missionary)
George Dana Boardman (February 8, 1801 – February 11, 1831) was an American missionary.
# Life.
He was born in Livermore, Maine, the son of the Rev. Sylvanus Boardman. He attended Colby College, and was the school's first graduate in 1822. He served as tutor for a year at Colby, then continued his education at Andover Theological Seminary. On February 16, 1825, he was ordained a Baptist minister in West Yarmouth, Maine. Rev. Jeremiah Chaplin, President of Colby College, spoke at his ordination. Boardman married Sarah Hall on July 4, 1825.
On July 16, the couple sailed for Calcutta, where they arrived on 2 December 1825. After acquiring the Burmese language, he | 17,502 |
1402476 | George Boardman (missionary) | https://en.wikipedia.org/w/index.php?title=George%20Boardman%20(missionary) | George Boardman (missionary)
entered upon his labors at Maulmain in May 1827, and founded a mission which became the central point of all the Baptist missions in Burma. In April 1828, he established a mission at Tavoy, where he soon afterward baptized Ko-mah-byn, a Karen convert, whose labors were very successful among his countrymen. On 5 February 1828, Boardman set out on a tour among the Karen villages, and met with such success that he determined on a systematic course of itinerary labor. On these trips, he was usually accompanied by Ko-mah-byn or some other convert.
His exertions occasioned the loss of his health and brought on his early death by consumption. His widow married the Rev. Adoniram Judson, also a missionary. | 17,503 |
1402476 | George Boardman (missionary) | https://en.wikipedia.org/w/index.php?title=George%20Boardman%20(missionary) | George Boardman (missionary)
s early death by consumption. His widow married the Rev. Adoniram Judson, also a missionary. He and Sarah had a son also named George Dana Boardman, often referred to as "the Younger".
A residence and dining hall at his alma mater, Colby College, is named "Dana" in his honor.
# References.
- Attribution
# Further reading.
- King, Alonzo (1834) "Memoir of George Dana Boardman : late missionary to Burmah, containing much intelligence relative to the Burman mission". Boston : Lincoln, Edmands & Co.
- Chaplin, Jeremiah (1825) "A Sermon Preached at North Yarmouth, February 16, 1825 : at the ordination of the Rev. George D. Boardman, as a missionary to the heathen". Waterville : W. Hastings. | 17,504 |
1402256 | Sir Anthony Meyer, 3rd Baronet | https://en.wikipedia.org/w/index.php?title=Sir%20Anthony%20Meyer,%203rd%20Baronet | Sir Anthony Meyer, 3rd Baronet
Sir Anthony Meyer, 3rd Baronet
Sir Anthony John Charles Meyer, 3rd Baronet (27 October 1920 – 24 December 2004) was a British soldier, diplomat, and Conservative and later Liberal Democrat politician, best known for standing against Margaret Thatcher for the party leadership in 1989. In spite of his staunch conservative views on economic policy, his passionate support of increased British integration into the European Union led to him becoming increasingly marginalised in Thatcher's Conservative Party.
After being deselected as a Conservative parliamentary candidate for the 1992 general election, Meyer became policy director of the European Movement, and in 1998 he joined the Pro-Euro Conservative | 17,505 |
1402256 | Sir Anthony Meyer, 3rd Baronet | https://en.wikipedia.org/w/index.php?title=Sir%20Anthony%20Meyer,%203rd%20Baronet | Sir Anthony Meyer, 3rd Baronet
Party. After that disbanded in 2001, he became a member of the Liberal Democrats.
# Early life.
Meyer was the son of Marjorie Amy Georgina (née Seeley) and Sir Frank Cecil Meyer. His father was vice-chairman of the De Beers diamond company, and from 1924 to 1929 he was Conservative Member of Parliament for Great Yarmouth, Norfolk. His father was from a Jewish family. His grandfather, Sir Carl Ferdinand Meyer, was born in Hamburg, Germany; he migrated to Britain in the late 19th century, when he worked for the Rothschilds, and later for De Beers; he eventually became Governor of the National Bank of Egypt and was given a baronetcy for the large donations he made to found a National Theatre | 17,506 |
1402256 | Sir Anthony Meyer, 3rd Baronet | https://en.wikipedia.org/w/index.php?title=Sir%20Anthony%20Meyer,%203rd%20Baronet | Sir Anthony Meyer, 3rd Baronet
in Britain.
## Education and war service.
Meyer was educated at Eton College, like his father, and he inherited the baronetcy at the age of 15 when his father died in a hunting accident. Like his father, he also attended New College, Oxford, but after one year he joined the Scots Guards in 1941, the same year he married Barbadee Knight, and they would have one son and three daughters. During the battle for Caen, in the break-out from the Normandy invasion beaches he was seriously wounded when the tank he was travelling in was hit, and he spent the next nine months on his back in hospital. During this time he read extensively to make up for his lost years at Oxford, but decided not to return | 17,507 |
1402256 | Sir Anthony Meyer, 3rd Baronet | https://en.wikipedia.org/w/index.php?title=Sir%20Anthony%20Meyer,%203rd%20Baronet | Sir Anthony Meyer, 3rd Baronet
to university. Instead, he joined HM Treasury where he mostly worked on winding up the affairs of the Polish government-in-exile.
## Diplomatic career.
In 1946 Meyer passed the Foreign Service examinations, and from 1951 to 1956 he was appointed to the British Embassy in Paris, where he became First Secretary in 1953. The subsequent appointment to the embassy in Moscow was not so enjoyable – he did not speak the language, and confined to the "diplomatic ghetto" through the Soviet government's ban on foreign contacts with its citizens, he said he did not have a job to do. He was rescued by a Soviet attempt to compromise him – he reported an attempt to lure him into a cab by a woman agent to | 17,508 |
1402256 | Sir Anthony Meyer, 3rd Baronet | https://en.wikipedia.org/w/index.php?title=Sir%20Anthony%20Meyer,%203rd%20Baronet | Sir Anthony Meyer, 3rd Baronet
the ambassador, who put Meyer and his family on the next plane home. Between 1958 and 1962, he worked at the Foreign Office on European political problems, at a time when the Office was changing its policy from being against the "Common Market" to in favour of Britain's joining it.
# Political career.
## Finding a party, and a seat.
The death of his mother in 1962 provided Meyer with the family's wealth, and he decided to enter politics to support his pro-European views. In 1962, he resigned from the Foreign Office to work unpaid for the Common Market Campaign led by Liberal peer Gladwyn Jebb, 1st Baron Gladwyn. He later said that he was initially undecided whether to stand for the Conservatives | 17,509 |
1402256 | Sir Anthony Meyer, 3rd Baronet | https://en.wikipedia.org/w/index.php?title=Sir%20Anthony%20Meyer,%203rd%20Baronet | Sir Anthony Meyer, 3rd Baronet
or the Liberals, but his admiration for the Conservative prime minister Harold Macmillan swung his choice.
In 1963, Meyer was selected to fight the constituency of Eton and Slough, then held by Labour's leftwing internationalist Fenner Brockway. In the 1964 General Election, Meyer won the seat by 11 votes, gaining respect by ignoring his constituency party's advice to campaign on the race issue, which could have swung a number of votes in that constituency at the time. His was one of only four Conservative gains in that election. Recognising that he would only be in the seat temporarily, Meyer made the most of his time in Parliament, advocating Britain's joining the Common Market and strengthening | 17,510 |
1402256 | Sir Anthony Meyer, 3rd Baronet | https://en.wikipedia.org/w/index.php?title=Sir%20Anthony%20Meyer,%203rd%20Baronet | Sir Anthony Meyer, 3rd Baronet
the United Nations. He also established himself on the liberal wing of the party: voting to abolish capital punishment and for sanctions against Rhodesia. In the 1966 General Election he lost his seat to Labour's Joan Lestor by 4,663 votes.
His liberalism made him almost untouchable in the Conservative party, and his applications to stand in six constituencies (including Windsor, where he lived) were rejected, but eventually fellow Old Etonian Nigel Birch recommended Meyer to replace him in the constituency of West Flintshire, in north-eastern Wales. He returned to Parliament at the 1970 General Election.
## MP for West Flintshire.
Meyer became a popular MP in his new constituency, gaining | 17,511 |
1402256 | Sir Anthony Meyer, 3rd Baronet | https://en.wikipedia.org/w/index.php?title=Sir%20Anthony%20Meyer,%203rd%20Baronet | Sir Anthony Meyer, 3rd Baronet
a reputation for putting the interests of his constituency ahead of Conservative government policy, for example by voting against the closure of the Shotton steelworks, supporting the Airbus A300B whose wings some of his constituents built, against its all-British rival the BAC 3-11, while insisting on the importance of an effective pan-European technology. After Labour's return to power in 1974, he opposed continued sanctions against the white minority government in Rhodesia, claiming that it was intended to transfer power "forcibly to a violent minority".
When the Conservative party returned to power under Margaret Thatcher in 1979, Meyer's type of pro-Europeanism was at odds with the Euroscepticism | 17,512 |
1402256 | Sir Anthony Meyer, 3rd Baronet | https://en.wikipedia.org/w/index.php?title=Sir%20Anthony%20Meyer,%203rd%20Baronet | Sir Anthony Meyer, 3rd Baronet
of the bulk of the party. When his Flintshire West constituency's boundaries were expanded and redrawn to form the Clwyd North West constituency in 1983, there was an attempt by local party activists to replace him with the more Thatcherite MEP, Beata Brookes, whom Meyer managed to defeat.
## Leadership challenge.
On 23 November 1989, at a time of both Thatcher's and the Conservative Party's waning popularity and shortly after Nigel Lawson's resignation as chancellor, 69-year-old Meyer put himself forward as the pro-European stalking horse for the leadership of the Conservative Party. Meyer fully expected that one of the more prominent pro-Europeans such as Ian Gilmour or Michael Heseltine | 17,513 |
1402256 | Sir Anthony Meyer, 3rd Baronet | https://en.wikipedia.org/w/index.php?title=Sir%20Anthony%20Meyer,%203rd%20Baronet | Sir Anthony Meyer, 3rd Baronet
would take over the role; in the event, none of them did so, and Meyer had no illusions that he had any chance of success. He was derided as "Sir Anthony Whats'isname" by the pro-Thatcher "Sun" newspaper, who reported that he was the only Conservative MP to oppose the use of force to win back the Falkland Islands following the Argentine invasion of 1982 and had backed a number of Labour policies, including votes against Tory-led welfare benefit cuts and immigration issues. He was also slammed by the "Daily Express" as "Sir Nobody".
In the 1989 leadership election on 5 December, Meyer was defeated by 314 votes to 33, but when spoilt votes and abstentions were added it was discovered that 60 | 17,514 |
1402256 | Sir Anthony Meyer, 3rd Baronet | https://en.wikipedia.org/w/index.php?title=Sir%20Anthony%20Meyer,%203rd%20Baronet | Sir Anthony Meyer, 3rd Baronet
MPs out of 374 had failed to support Thatcher. Meyer said that "people started to think the unthinkable", and Thatcher was ousted in November 1990 to be succeeded by John Major.
On 19 January 1990, Meyer was deselected as a candidate for the 1992 general election by the Clwyd North West constituency party for his "treachery", by a 2–1 majority. The deselection campaign was enlivened by a tabloid newspaper's revelation that Meyer had for 26 years had an affair with Simone Washington, a former model and blues singer.
# Post-parliamentary career.
After his forced career change in 1992 Meyer became policy director for the European Movement, and in 1998 he defected to the Pro-Euro Conservative | 17,515 |
1402256 | Sir Anthony Meyer, 3rd Baronet | https://en.wikipedia.org/w/index.php?title=Sir%20Anthony%20Meyer,%203rd%20Baronet | Sir Anthony Meyer, 3rd Baronet
Party before becoming a member of the Liberal Democrats. In 1999 he stood unsuccessfully, during the European Parliament elections, for the London seat. After 1999 he became a lecturer on European affairs until his death.
# Death.
Meyer died of cancer, aged 84, in Kensington and Chelsea, London, in December 2004.
His son, Anthony Ashley Frank Meyer, (born 1944), succeeded him in the baronetcy.
# In popular culture.
Meyer was portrayed by Geoffrey Wilkinson in the 2002 BBC production of Ian Curteis' controversial "The Falklands Play".
# External links.
- Obituary – Sir Anthony Meyer "The Guardian", 8 January 2005
- Obituary – Sir Anthony Meyer "Times Online", 8 January 2005
- Obituary | 17,516 |
1402256 | Sir Anthony Meyer, 3rd Baronet | https://en.wikipedia.org/w/index.php?title=Sir%20Anthony%20Meyer,%203rd%20Baronet | Sir Anthony Meyer, 3rd Baronet
In 1999 he stood unsuccessfully, during the European Parliament elections, for the London seat. After 1999 he became a lecturer on European affairs until his death.
# Death.
Meyer died of cancer, aged 84, in Kensington and Chelsea, London, in December 2004.
His son, Anthony Ashley Frank Meyer, (born 1944), succeeded him in the baronetcy.
# In popular culture.
Meyer was portrayed by Geoffrey Wilkinson in the 2002 BBC production of Ian Curteis' controversial "The Falklands Play".
# External links.
- Obituary – Sir Anthony Meyer "The Guardian", 8 January 2005
- Obituary – Sir Anthony Meyer "Times Online", 8 January 2005
- Obituary – Sir Anthony Meyer "Daily Telegraph", 10 January 2005 | 17,517 |
1402182 | 1942 Atlantic hurricane season | https://en.wikipedia.org/w/index.php?title=1942%20Atlantic%20hurricane%20season | 1942 Atlantic hurricane season
1942 Atlantic hurricane season
The 1942 Atlantic hurricane season was one of seven seasons to feature multiple hurricane landfalls in Texas. The season officially lasted from June 16, 1942, to October 31, 1942. These dates conventionally delimit the period of each year when most tropical cyclones form in the Atlantic basin. A total of 11 tropical storms from 1943 are listed in the Atlantic hurricane database, with two additional tropical depressions. The first system of the year, a tropical depression, developed over the central Gulf of Mexico on June 3, while the last system, the Belize hurricane, dissipated over the Yucatán Peninsula on November 11. After the depression dissipated on June 3, | 17,518 |
1402182 | 1942 Atlantic hurricane season | https://en.wikipedia.org/w/index.php?title=1942%20Atlantic%20hurricane%20season | 1942 Atlantic hurricane season
the season remained dormant until the next system developed two months later. In mid-August, a hurricane struck Texas, causing about $790,000 (1942 USD) in damage.
The most significant tropical cyclone of the season, known as the Matagorda hurricane, developed on August 23. After striking the Yucatán Peninsula, the storm entered the Gulf of Mexico and intensified into a Category 3 hurricane on Saffir–Simpson scale, becoming the only major hurricane of the season. The hurricane devastated southern Texas, with damage as far inland as San Antonio. Eight fatalities and about $26.5 million in damage were reported. Several of the proceeding tropical systems left little impact on land, though the | 17,519 |
1402182 | 1942 Atlantic hurricane season | https://en.wikipedia.org/w/index.php?title=1942%20Atlantic%20hurricane%20season | 1942 Atlantic hurricane season
remnants of the ninth tropical storm contributed to severe flooding in Virginia. In November, a hurricane caused extensive impact in several coastal communities of Belize (then known as British Honduras). The hurricane left nine deaths and about $4 million in damage.
# Systems.
## Tropical Storm One.
On August 1, a low-pressure area was first detected in the vicinity of Puerto Cabezas, Nicaragua. However, data at the time was not conclusively indicative of a tropical cyclone. The tropical low was later analyzed to have sufficiently organized to be classified as a tropical depression by 0000 UTC on August 3, as it moved westward in the Gulf of Honduras. Six hours later, the depression was | 17,520 |
1402182 | 1942 Atlantic hurricane season | https://en.wikipedia.org/w/index.php?title=1942%20Atlantic%20hurricane%20season | 1942 Atlantic hurricane season
estimated to have intensified into a tropical storm based on barometric readings from Tela, Honduras, and Belize City. Shortly after, the tropical storm made landfall in British Honduras with winds of 40 mph (65 km/h). The tropical cyclone weakened to a tropical depression during its trek over the Yucatán Peninsula before emerging into the Bay of Campeche on August 4. Over water, the storm reintensified and attained its peak intensity with winds of 60 mph (95 km/h) at 0600 UTC on the following day . Three hours later, the storm made its final landfall south of Tampico, Mexico, at the same intensity, before weakening over the mountainous terrain of Mexico and dissipating late on August 5.
Upon | 17,521 |
1402182 | 1942 Atlantic hurricane season | https://en.wikipedia.org/w/index.php?title=1942%20Atlantic%20hurricane%20season | 1942 Atlantic hurricane season
landfall near Tampico, a station in the city recorded a minimum barometric pressure of 1,004 mbar (hPa; 29.65 inHg), the lowest pressure measured in association with the storm. Due to a lack of available weather ships in the region because of World War II, no ships documented the tropical cyclone. In Texas, the tropical cyclone caused light rainfall, damaging local cotton crops. Strong wind gusts were observed in the Rio Grande Valley.
## Hurricane Two.
A tropical wave developed into a tropical depression about east of the Yucatán Peninsula on August 17. Moving north-northwestward, the depression soon strengthened into a tropical storm. Early on August 18, the system crossed the Yucatán Channel | 17,522 |
1402182 | 1942 Atlantic hurricane season | https://en.wikipedia.org/w/index.php?title=1942%20Atlantic%20hurricane%20season | 1942 Atlantic hurricane season
and entered the Gulf of Mexico. While nearing the coast of Louisiana on August 19, the storm slowed down, turned westward, and intensified into a Category 1 hurricane. Late on August 19, the hurricane attained its maximum sustained wind speed of 80 mph (130 km/h). The cyclone curved west-northwestward and weakened slightly before making landfall near Crystal Beach, Texas, with winds of 75 mph (120 km/h) around 13:00 UTC on August 21. At landfall, the barometric pressure fell to based on the pressure-wind relationship – the lowest pressure associated with the storm. The hurricane weakened after moving inland, falling to tropical storm status less than five hours later and to tropical depression | 17,523 |
1402182 | 1942 Atlantic hurricane season | https://en.wikipedia.org/w/index.php?title=1942%20Atlantic%20hurricane%20season | 1942 Atlantic hurricane season
intensity early on August 22. The system then curved northeastward and became extratropical over the Arkansas–Missouri state line, shortly before the remnants dissipated.
In Texas, tides reached above mean low water at High Island. The abnormally high tides damaged piers and small crafts, while two barges and a tow boat also collapsed. Strong winds were reported in some areas, with sustained winds of observed in Port Arthur. Trees and power lines were downed throughout the city, while trees and signs were toppled in Beaumont. On the Bolivar Peninsula, three oil derricks were toppled. More than 50% of customers of the Gulf States Electrical Company were left without power. In Henderson, winds | 17,524 |
1402182 | 1942 Atlantic hurricane season | https://en.wikipedia.org/w/index.php?title=1942%20Atlantic%20hurricane%20season | 1942 Atlantic hurricane season
unroofed a number of homes and destroyed a few others. The hurricane dropped up to of rainfall. Near Hallsville, about of the Texas and Pacific Railway was washed out. Precipitation destroyed about 15% of rice crops in Jefferson County. Overall, damage reached approximately $790,000.
## Hurricane Three.
The Matagorda Hurricane of 1942
A tropical wave developed into a tropical depression over the central Caribbean Sea around 12:00 UTC on August 23. Trekking west-northwestward, the system strengthened into a tropical storm about 24 hours later. It gradually intensified, and reach hurricane status south of Jamaica on August 25. The hurricane then curved northwest and intensified into a Category 2 | 17,525 |
1402182 | 1942 Atlantic hurricane season | https://en.wikipedia.org/w/index.php?title=1942%20Atlantic%20hurricane%20season | 1942 Atlantic hurricane season
hurricane on August 27. Early the following day, the cyclone made landfall near Cancún, Quintana Roo, with winds of 105 mph (165 km/h). The storm weakened to a Category 1 during its brief transit across the Yucatán Peninsula, before re-intensifying into a Category 2 hurricane over the Gulf of Mexico late on August 28. The hurricane quickly strengthened, and attained its peak intensity on August 29 as a Category 3 hurricane with winds of 115 mph (185 km/h). However, nearing the Texas Gulf Coast, the storm waned in intensity, and was only a Category 1 hurricane by the time it made a final landfall near Matagorda, Texas, on August 30. Continuing inland, the hurricane weakened, and degenerated into | 17,526 |
1402182 | 1942 Atlantic hurricane season | https://en.wikipedia.org/w/index.php?title=1942%20Atlantic%20hurricane%20season | 1942 Atlantic hurricane season
a remnant low over New Mexico on August 31.
At the hurricane's first landfall near the northeastern tip of the Yucatán Peninsula, little information was documented on the storm's impacts. However, as the storm approached the Texas coast, widespread evacuations took place, including the evacuation of roughly 50,000 people from Galveston alone. Upon making landfall, the hurricane caused extensive damage in coastal regions. In Matagorda, storm surge peaking at 14.7 ft (4.5 m) inundated the city and damaged many others. Strong winds from the storm wreaked havoc as far inland as San Antonio. The winds leveled numerous buildings and uprooted trees, in addition to causing widespread power outages. | 17,527 |
1402182 | 1942 Atlantic hurricane season | https://en.wikipedia.org/w/index.php?title=1942%20Atlantic%20hurricane%20season | 1942 Atlantic hurricane season
Crops in the areas affected saw large losses, particularly the rice crop. Rainfall associated with the storm was relatively light, due to the hurricane's rapid forward motion once inland, peaking at 9.3 in (0.24 mm) in Woodsboro. Overall, the storm caused $26.5 million in damages and eight deaths.
## Hurricane Four.
The fourth tropical storm of the season was first detected as a minimal hurricane about 355 mi (570 km) southeast of Bermuda on August 25. Due to lack of data, little further information is known about the origin of this system. Historical weather maps showed a tropical storm on August 24, though there was insufficient evidence of a closed circulation. The hurricane moved north-northwestward | 17,528 |
1402182 | 1942 Atlantic hurricane season | https://en.wikipedia.org/w/index.php?title=1942%20Atlantic%20hurricane%20season | 1942 Atlantic hurricane season
and intensified into a Category 2 hurricane early on August 26. The storm then made its closest approach to Bermuda, passing about east of island, which observed a sustained wind speed of . At 06:00 UTC on August 26, the cyclone peaked with maximum sustained winds of 110 mph (175 km/h). The hurricane produced sustained winds of . The system slowly weakened as it continued northeastward, falling to Category 1 intensity early on August 28 and deteriorating to a tropical storm late on August 29. Around that time, the cyclone decelerated and curved to the southwest. Early on September 3, the system weakened to a tropical depression, several hours before dissipating about east-northeast of Bermuda.
## | 17,529 |
1402182 | 1942 Atlantic hurricane season | https://en.wikipedia.org/w/index.php?title=1942%20Atlantic%20hurricane%20season | 1942 Atlantic hurricane season
Tropical Storm Five.
The fifth tropical storm of the season formed on September 15 about 60 mi (95 km) southeast of Barbados. The system moved west-northwestward and passed between Saint Lucia and Saint Vincent early the next day. After entering the Caribbean, the cyclone slowly intensified and peaked with sustained winds of 50 mph (85 km/h) on September 17. The following day, the storm curved westward while located south of Hispaniola. While the system passed south of Jamaica, rough seas and sustained winds of were reported at Morant Point. On September 21, the storm tracked to the north of Great Swan Island, which observed a barometric pressure near , the lowest known pressure associated | 17,530 |
1402182 | 1942 Atlantic hurricane season | https://en.wikipedia.org/w/index.php?title=1942%20Atlantic%20hurricane%20season | 1942 Atlantic hurricane season
with the cyclone. Thereafter, the storm began to slowly weaken. Just after 12:00 UTC on September 22, the system made landfall in Stann Creek District in Belize as a minimal tropical storm. The cyclone soon weakened to a tropical depression and dissipated near the Guatemala–Mexico border around 24 hours after moving inland.
## Tropical Storm Six.
A low pressure area developed into a tropical storm around 12:00 UTC on September 18, while located about north of Bermuda. The storm moved southwestward and passed northwest of the island, which observed sustained winds of . Late on September 19, the cyclone curved northwestward. The system intensified to reach maximum sustained winds of 50 mph (85 km/h) | 17,531 |
1402182 | 1942 Atlantic hurricane season | https://en.wikipedia.org/w/index.php?title=1942%20Atlantic%20hurricane%20season | 1942 Atlantic hurricane season
and a minimum barometric pressure of on September 20. Early the next day, the cyclone curved northeastward and began losing tropical characteristics. By 00:00 UTC on September 22, the system had already completed its transition to an extratropical cyclone while located about 275 mi (445 km) southeast of Nantucket, Massachusetts. The extratropical remnants continued northeastward, striking Newfoundland before dissipating early on September 25.
## Tropical Storm Seven.
A low pressure area developed into a tropical storm about 185 mi (300 km) south-southeast of Bermuda early on September 27. On the following day, the storm's barometric pressure decreased to – the lowest known pressure associated | 17,532 |
1402182 | 1942 Atlantic hurricane season | https://en.wikipedia.org/w/index.php?title=1942%20Atlantic%20hurricane%20season | 1942 Atlantic hurricane season
with the system. Moving west-northwestward, the cyclone produced winds of on Bermuda on September 28. Several hours later, the system began to move north-northwestward. Early on September 29, the storm attained its maximum sustained wind speed of 50 mph (85 km/h). However, by 12:00 UTC, the cyclone merged with a cold front about northwest of Bermuda.
## Tropical Storm Eight.
On September 30, the next system developed north of the Turks and Caicos Islands. Initially a tropical depression, the cyclone intensified into a tropical storm early on October 1. Around 17:00 UTC, a ship recorded a barometric pressure of , which was reanalyzed as , the lowest pressure associated with the storm. The storm | 17,533 |
1402182 | 1942 Atlantic hurricane season | https://en.wikipedia.org/w/index.php?title=1942%20Atlantic%20hurricane%20season | 1942 Atlantic hurricane season
continued northeastward and reached maximum sustained winds of 70 mph (110 km/h) by October 2. On the following day, the system passed to the southeast of Bermuda, which observed sustained winds up to . Due to lack of data, it is possible the storm intensified into a hurricane before completing the transition into an extratropical cyclone about south of Newfoundland on October 4. The remnant system continued northeastward until dissipating east of Newfoundland late on October 5.
## Tropical Storm Nine.
A tropical storm was first observed about midway between the Abaco Islands and Bermuda early on October 10. However, the storm was short lived.
Around 06:00 UTC on the following day, the cyclone | 17,534 |
1402182 | 1942 Atlantic hurricane season | https://en.wikipedia.org/w/index.php?title=1942%20Atlantic%20hurricane%20season | 1942 Atlantic hurricane season
reached maximum sustained winds of 45 mph (75 km/h). Only six hours later, the system lost tropical characteristics while located about , after the vortex became elongated while a frontal system approached the area. The remnants continued northwestward and moved ashore in North Carolina early on October 12, before dissipating early the following day.
Heavy rainfall was reported in northeastern North Carolina. The remnants contributed to severe flooding in northern Virginia. Although the remnant system dissipated by October 13, moisture laden-air brought by the system and persistent easterly winds resulted in orographic lift, causing four days of record rainfall. The Big Meadows area of Shenandoah | 17,535 |
1402182 | 1942 Atlantic hurricane season | https://en.wikipedia.org/w/index.php?title=1942%20Atlantic%20hurricane%20season | 1942 Atlantic hurricane season
National Park observed of precipitation, while rainfall totals above were common. Madison County recorded of precipitation in only 24 hours. Numerous highways were washed out and many bridges were swept away, interrupting traffic for three to four days. Severe damage to crops occurred. About 1,300 people were left homeless in Albemarle, Spotsylvania, Stafford, and Warren counties. In the Washington, D.C. area, the rising Potomac River forced the evacuation of 722 families. Several homes were swept from their foundation, while hundreds of others were flooded in Georgetown. Minor damage occurred at the Washington Navy Yard. Maine Avenue was inundated with about of water. One death occurred during | 17,536 |
1402182 | 1942 Atlantic hurricane season | https://en.wikipedia.org/w/index.php?title=1942%20Atlantic%20hurricane%20season | 1942 Atlantic hurricane season
the flood.
## Tropical Storm Ten.
A tropical depression developed just offshore modern-day Granma Province in Cuba on October 13, moving ashore within six hours. After emerging into the Atlantic near Gibara early on October 14, the depression turned northward and soon intensified into a tropical storm. During the next 24 hours, the storm moved through the central Bahamas, striking or passing close to the islands of Exuma, Little San Salvador, and Eleuthera. A barometric pressure of was observed on Eleuthera around 12:00 UTC on October 15, which was the lowest known pressure in relation to the system. The storm then turned northeastward and continued to slowly strengthen, peaking with maximum | 17,537 |
1402182 | 1942 Atlantic hurricane season | https://en.wikipedia.org/w/index.php?title=1942%20Atlantic%20hurricane%20season | 1942 Atlantic hurricane season
sustained winds of 50 mph (85 km/h) on October 16. By late on October 18, the cyclone merged with a cold front while situated about 305 mi (490 km) southeast of Massachusetts.
## Hurricane Eleven.
A tropical wave developed into a tropical depression over the Turks and Caicos Islands on November 5. The cyclone strengthened slowly while moving westward and then south-southwestward across the Bahamas. On November 6, the storm became a Category 1 hurricane. Later that day, it made landfall in Cuba near Cayo Romano, Camagüey Province, with winds of 80 mph (130 km/h). Impact in Cuba and the Bahamas was generally limited to lower barometric pressure readings and strong winds. While crossing Cuba, | 17,538 |
1402182 | 1942 Atlantic hurricane season | https://en.wikipedia.org/w/index.php?title=1942%20Atlantic%20hurricane%20season | 1942 Atlantic hurricane season
the system weakened to a tropical storm early on November 7, shortly before emerging into the Caribbean Sea. The storm re-strengthened into a hurricane later that day and headed southwestward.
Late on November 8, the hurricane curved westward and intensified into a Category 2 hurricane. Six hours later, it peaked with maximum sustained winds of 110 mph (175 km/h). Early on November 9, the storm struck Caye Caulker and northern Belize District. Rapidly weakening, the system fell to tropical storm status within 12 hours of landfall. By early on November 10, it emerged into the Bay of Campeche. The storm meandered erratically until striking the Yucatán Peninsula on November 11 and dissipating | 17,539 |
1402182 | 1942 Atlantic hurricane season | https://en.wikipedia.org/w/index.php?title=1942%20Atlantic%20hurricane%20season | 1942 Atlantic hurricane season
hours later. Strong winds were observed in Belize and Mexico's Yucatán Peninsula. Severe damage was reported in the former. About 90% of structures in San Pedro Town were destroyed, while Newtown was completely obliterated, causing its residents to relocate and establish the village of Hopkins. Trees and crops such as coconuts also suffered heavy losses. Overall, nine deaths and approximately $4 million in damage were reported.
## Other systems.
In addition to the 11 tropical storms, 2 other systems that remained below tropical storm intensity developed. The first such system developed from a low pressure area over the eastern Gulf of Mexico on June 3. The depression moved rapidly northwestward | 17,540 |
1402182 | 1942 Atlantic hurricane season | https://en.wikipedia.org/w/index.php?title=1942%20Atlantic%20hurricane%20season | 1942 Atlantic hurricane season
ensity developed. The first such system developed from a low pressure area over the eastern Gulf of Mexico on June 3. The depression moved rapidly northwestward toward Louisiana, before transitioning into an extratropical cyclone by the following day. A barometric pressure of was observed in Lake Charles, Louisiana, while a sustained wind speed of was recorded in Apalachicola, Florida. On October 15, a tropical depression formed just east of the Lesser Antilles. The depression moved northward and avoided landfall in the islands. The depression dissipated by October 18.
# See also.
- List of tropical cyclones
- List of Atlantic hurricane seasons
# External links.
- Monthly Weather Review | 17,541 |
1402267 | 1941 Atlantic hurricane season | https://en.wikipedia.org/w/index.php?title=1941%20Atlantic%20hurricane%20season | 1941 Atlantic hurricane season
1941 Atlantic hurricane season
The 1941 Atlantic hurricane season was the period during 1941 in which tropical cyclones formed in the Atlantic Basin. It was a relatively inactive hurricane season, with only six known storms. It officially began on June 16, 1941, and lasted until November 1, 1941. These dates delimit the period of each year when most tropical cyclones tend to form in the Atlantic basin. Of the six cyclones, four attained hurricane status, and three became major hurricanes. The active season had an abnormally late start; the first system formed on September 11, nearly three months after the official beginning date. The season was also short-lived, as all six storms developed in | 17,542 |
1402267 | 1941 Atlantic hurricane season | https://en.wikipedia.org/w/index.php?title=1941%20Atlantic%20hurricane%20season | 1941 Atlantic hurricane season
rapid succession. On September 23, three hurricanes existed simultaneously in the Atlantic basin.
In total, the season resulted in about 63 fatalities and over $10 million in damages. The first and last storms of the season were largely insignificant, although the second, fourth, and fifth storms had considerable effects. Two hurricanes struck the United States: a major hurricane that struck Texas and Louisiana in late September, disrupting the Louisiana Maneuvers, and Hurricane Five, which made two landfalls in Florida, the first of which was near Miami at Category 2 intensity, inflicting widespread damage. Another major storm—Hurricane Four—traversed the Caribbean before striking the Nicaragua–Honduras | 17,543 |
1402267 | 1941 Atlantic hurricane season | https://en.wikipedia.org/w/index.php?title=1941%20Atlantic%20hurricane%20season | 1941 Atlantic hurricane season
border at Category 4 intensity, leaving 47 men dead at sea.
# Systems.
## Tropical Storm One.
The first storm of the 1941 season formed on September 11 in the northern Gulf of Mexico. This was an abnormally late start to an Atlantic hurricane season: only on two other occasions between 1887 and 1941 had no storms developed prior to September 11. The storm moved slowly in a generally westward direction for the next few days, peaking as a moderate tropical storm with winds of 45 mph (75 km/h). It then weakened until it made landfall along the northern Texas coast between Galveston and Port Arthur as a tropical depression, where it caused only minor damage. Near 0600 UTC on September 16, the | 17,544 |
1402267 | 1941 Atlantic hurricane season | https://en.wikipedia.org/w/index.php?title=1941%20Atlantic%20hurricane%20season | 1941 Atlantic hurricane season
storm deteriorated into a depression, and dissipated a few hours later.
## Hurricane Two.
The Texas Hurricane of 1941
Little more than a day after the first storm of the season dissipated, a tropical depression formed on September 17 in the central Gulf of Mexico about north of the Yucatán Peninsula. Upon forming, the system began moving generally northward. Early on September 18, the system developed into a tropical storm more than to the south-southeast of New Orleans, Louisiana. Over the next three days, the intensifying storm executed a gradual clockwise loop, moving to the south-southeast before turning back to the west. After intensifying to a Category 1 hurricane on September 21, the | 17,545 |
1402267 | 1941 Atlantic hurricane season | https://en.wikipedia.org/w/index.php?title=1941%20Atlantic%20hurricane%20season | 1941 Atlantic hurricane season
storm began assuming a more northwestward course, toward the Texas Gulf Coast. It continued to strengthen into a major hurricane, peaking at late on September 23. About four hours later, at about 22 UTC, the storm went ashore east of Bay City, Texas, on September 23. The estimated minimum central pressure fell to as low as . It curved towards the northeast, passing just east of Houston, and accelerated as it continued to move inland. The cyclone transitioned into an extratropical storm on September 25, and was last recorded at 00 UTC on September 27 over northeastern Quebec, near the Torngat Mountains National Park.
Warnings and advisories declared in response to the storm were widely distributed, | 17,546 |
1402267 | 1941 Atlantic hurricane season | https://en.wikipedia.org/w/index.php?title=1941%20Atlantic%20hurricane%20season | 1941 Atlantic hurricane season
and approximately 25,000 people in the area evacuated their homes. Officials completed various precautionary measures. Wind gusts along the coast reached up to , and high storm tides were recorded. The hurricane inflicted severe damage; destruction to property was worth an estimated $2 million, with an additional $5 million in damage to crops, notably rice and cotton. Overall, the cyclone killed four people. The hurricane affected the southern Louisiana region one week before the Louisiana Maneuvers, a prelude to World War II. Heavy rainfall triggered flooding and swelled rivers, and army vehicles became stuck in the mud as a result. The inclement weather forced hundreds of military aircraft | 17,547 |
1402267 | 1941 Atlantic hurricane season | https://en.wikipedia.org/w/index.php?title=1941%20Atlantic%20hurricane%20season | 1941 Atlantic hurricane season
to move inland for shelter.
## Hurricane Three.
Early on September 18, squally weather was reported throughout the Atlantic coast of Florida, with indications that a circulation center was present offshore. It is estimated that a tropical storm had formed at around this time. The cyclone began to intensify as it briefly moved northeastward, before abruptly executing an eastward turn. It attained Category 1 hurricane status on September 19, and completed a clockwise loop the next day. It then tracked northwestward toward North Carolina, but began to recurve away from land late on September 22. It weakened into a tropical storm shortly afterward. The system dissipated on September 25 to the | 17,548 |
1402267 | 1941 Atlantic hurricane season | https://en.wikipedia.org/w/index.php?title=1941%20Atlantic%20hurricane%20season | 1941 Atlantic hurricane season
south of Nova Scotia. The storm had little or no effect on land, but caused significant delays for North Atlantic shipping. One vessel en route from Curaçao to New York encountered the storm on two separate occasions, recording Force 8 winds on the Beaufort scale both times.
## Hurricane Four.
The Nicaragua Hurricane of 1941
On September 23, a minor area of disturbed weather was observed about to the northwest of Barbados. It is estimated that it developed into a tropical storm shortly thereafter. Tracking westward, it passed just south of St. Lucia and emerged into the Caribbean Sea. By September 25, the storm had reached hurricane strength. Still intensifying, the storm continued generally | 17,549 |
1402267 | 1941 Atlantic hurricane season | https://en.wikipedia.org/w/index.php?title=1941%20Atlantic%20hurricane%20season | 1941 Atlantic hurricane season
westward and reached its peak at Category 4 on the Saffir-Simpson Hurricane Scale. By late September 27, the hurricane was situated near Cape Gracias a Dios, Honduras, and accelerated as it moved across the northernmost stretch of the country. It maintained hurricane intensity despite moving over mountainous terrain. After briefly entering the Gulf of Honduras, it moved ashore again in Belize, with winds of up to . Gradually weakening, the storm continued inland and weakened to a tropical storm by September 29. The storm emerged over the Bay of Campeche as a tropical depression and dissipated on September 30 while over water.
Approximately 47 lives were lost at sea due to the hurricane. The | 17,550 |
1402267 | 1941 Atlantic hurricane season | https://en.wikipedia.org/w/index.php?title=1941%20Atlantic%20hurricane%20season | 1941 Atlantic hurricane season
"SS Ethel Sakel" displayed a "sinking" message on September 25, about north of Aruba; she later went down with 20 of her 33 crew members. Two other ships sent out distress signals, one of which capsized, all hands lost. Damage on land was also extensive, and three people drowned at Cape Gracias, which was largely destroyed by the storm. Coastal flooding in the town was severe. Inland, a ship encountered the calm eye of the cyclone, and the barometric pressure aboard fell to ; the actual pressure at the coast was believed to have been far lower. In Belize, forests sustained major damage. For example, in the Melinda region, high winds brought down about 10% of the large pines.
## Hurricane Five.
The | 17,551 |
1402267 | 1941 Atlantic hurricane season | https://en.wikipedia.org/w/index.php?title=1941%20Atlantic%20hurricane%20season | 1941 Atlantic hurricane season
Florida Hurricane of 1941
Tropical Storm Five was first observed to the north of the Virgin Islands on October 3. The storm tracked generally westward on October 4, strengthening to its peak intensity of at 12 UTC the next day. Now a Category 3 hurricane on the modern-day Saffir-Simpson Hurricane Scale, the storm struck Cat Island, causing major damage. However, the rapidly moving storm soon weakened as its track bent more to the northwest. At 00 UTC on October 6, the eye of the storm passed south of Nassau. Ten hours later, the small hurricane struck the north end of Elliott Key, Florida, and then made a second landfall within the hour on the mainland at Goulds, near Homestead. Winds at landfall | 17,552 |
1402267 | 1941 Atlantic hurricane season | https://en.wikipedia.org/w/index.php?title=1941%20Atlantic%20hurricane%20season | 1941 Atlantic hurricane season
reached , and the calm eye was reported over Goulds. After moving across southern Florida, the storm had weakened to a strong tropical storm, but then restrengthened as it curved northwestward over the Gulf of Mexico. At about 09 UTC on October 7, the storm made another landfall along the Florida Panhandle near Carrabelle with winds of . Turning toward the north and northeast, it crossed Georgia and South Carolina, and entered the Atlantic Ocean on October 8. The storm fully dissipated several days later.
Preparations for the storm were extensive; residents boarded up homes and businesses, while evacuations were recommended in some coastal areas. In the Bahamas, where winds reached , the storm | 17,553 |
1402267 | 1941 Atlantic hurricane season | https://en.wikipedia.org/w/index.php?title=1941%20Atlantic%20hurricane%20season | 1941 Atlantic hurricane season
killed three people. The city of Nassau was struck particularly hard, though damage elsewhere in the islands was also severe, with many homes reported destroyed. In Florida, damage was relatively severe, and included the deaths of several people. High winds brought down trees and power lines, and wind-driven salt water damaged vegetation well inland across Dade County, though the storm was characterized by unusually light rainfall. Storm surge in the Everglades region flooded local streets, particularly at Everglades City. As the storm progressed northward, the city of Tallahassee suffered widespread power outages and damage to numerous vehicles. Throughout the state, the hurricane inflicted | 17,554 |
1402267 | 1941 Atlantic hurricane season | https://en.wikipedia.org/w/index.php?title=1941%20Atlantic%20hurricane%20season | 1941 Atlantic hurricane season
$675,000 (1941 USD) in damages. The cyclone later killed one person in Georgia.
## Tropical Storm Six.
A tropical storm formed on October 15, and passed through the southern Bahamas. It crossed the Florida Straits, and reached its peak intensity with winds of 50 mph (85 km/h) on October 20, after entering the eastern Gulf of Mexico and turning towards the north. It curved northeastward and made landfall at Cedar Key, Florida. After pushing inland, the storm stalled and weakened to a tropical depression on October 21 before dissipating fully the next day.
The storm's slow forward motion over the state of Florida led to heavy widespread precipitation, locally amounting to in Trenton, Florida | 17,555 |
1402267 | 1941 Atlantic hurricane season | https://en.wikipedia.org/w/index.php?title=1941%20Atlantic%20hurricane%20season | 1941 Atlantic hurricane season
lorida. After pushing inland, the storm stalled and weakened to a tropical depression on October 21 before dissipating fully the next day.
The storm's slow forward motion over the state of Florida led to heavy widespread precipitation, locally amounting to in Trenton, Florida between October 17 and October 22. Gale-force winds were also reported. Some flood damage occurred throughout the affected locations. An infant was killed following the destruction of a house, possibly related to a tornado spawned by the tropical storm; the baby's parents also sustained injuries.
# See also.
- List of Atlantic hurricane seasons
- List of tropical cyclones
# External links.
- Monthly Weather Review | 17,556 |
1402494 | Honda VFR800 | https://en.wikipedia.org/w/index.php?title=Honda%20VFR800 | Honda VFR800
Honda VFR800
The Honda VFR800 (Interceptor in the US after 2002) is a sport touring motorcycle made by Honda since 1998. The model was the successor to the VFR750F and shares the V4 engine configuration with the Honda VF and VFR series.
## 1998–2001 VFR800Fi (RC46).
Rather than being a direct development of the previous, carbureted VFR750F engine, the VFR800 engine was a detuned and longer-stroke power plant based on the fuel-injected engine designed for the RC45 of 1994. The RVF750R RC45 engine, although a development of the VFR750R RC30 and originally derived from the VFR750F RC24, was very different from Honda's previous V4s as the gear drive for the camshafts was moved from the centre | 17,557 |
1402494 | Honda VFR800 | https://en.wikipedia.org/w/index.php?title=Honda%20VFR800 | Honda VFR800
of the engine to the engine's right-side (next to the clutch-pack). Another change was the two side-mounted radiators as opposed to just one at the engine front like in the VFR750. The engine was tuned for road use in the VFR800, so that torque was improved throughout the rev range while maximum power was only slightly higher than the VFR750.
The VFR800's frame, which uses the engine as a stressed member, was derived from the VTR1000 Firestorm, retains the trademark VFR single-sided swingarm though, pivoted from the aft of the crankcase. It uses normal 'right-side-up' front forks.
In 2000, Honda updated the fifth-generation VFR (RC46) with a catalytic converter, oxygen sensors, and an EFI | 17,558 |
1402494 | Honda VFR800 | https://en.wikipedia.org/w/index.php?title=Honda%20VFR800 | Honda VFR800
system that would enter closed-loop mode under highway (cruising) operation. These also came with a temperature-actuated fast idle system, negating the need for a choke lever. The rear-view mirrors got updated as well, with Honda forgoing the old rubberized stalks, instead opting for rustproof metal ones. Bikes supplied for Europe also came with the H.I.S.S. (Honda Ignition Security System) immobiliser system in an effort to combat theft.
### Dual combined braking system (DCBS).
The VFR800 has a DCBS linked braking system. This is a departure from traditional motorcycle braking system where front and rear braking are independent of each other. In this system, the front brake lever applies | 17,559 |
1402494 | Honda VFR800 | https://en.wikipedia.org/w/index.php?title=Honda%20VFR800 | Honda VFR800
pressure to four (or later, five) of the six front brake caliper pistons. The rotational movement of the left caliper when engaged actuates a secondary master cylinder and applies pressure to one of the rear caliper's pistons. The rear brake pedal is directly attached to the remaining pistons (two in the rear, and one (or two) in the front).
The DCBS system is designated "Dual" as both hand lever and foot pedal each control both front and rear brakes; while commonly the foot pedal only operates the rear brake. Honda first introduced this braking system on the 1992 Honda CBR1000F. It was based on the Unified Braking System that was introduced on the 1983 GL1100.
## 2002–2013 VFR800 VTEC (RC46).
The | 17,560 |
1402494 | Honda VFR800 | https://en.wikipedia.org/w/index.php?title=Honda%20VFR800 | Honda VFR800
sixth generation VFR was introduced in 2002. It featured dual underseat exhausts, optional ABS, DCBS linked brakes, and optional hard luggage. It featured chain-driven cams rather than the gear-driven cams of earlier VFRs, and VTEC valve actuation.
The VFR800 was phased out after the 2009 model year in the United States, when Honda introduced the larger VFR1200F; but the VFR1200 was not a direct replacement for the VFR800; the true successor is the 2014 VFR800F (RC79). The RC46 model of VFR800 continues to be sold in certain international markets.
### VTEC valve actuation.
The VFR800 was the first non-JDM motorcycle to use VTEC valve-gear. Honda used VTEC to meet tightening noise and emissions | 17,561 |
1402494 | Honda VFR800 | https://en.wikipedia.org/w/index.php?title=Honda%20VFR800 | Honda VFR800
standards and to increase the peak engine horsepower.
Based on the VTEC-E system, the simplified motorcycle version of VTEC employs only two of the four valves per cylinder when operating at lower engine speeds. All four valves per cylinder are engaged above approximately 6,800 rpm. This is initiated by an electronically actuated oil spool valve, which sends oil pressure to the lifter actuators, which then move the engagement pins into place above the valve stem, allowing the remaining two valves to open. This design allows for variable valve timing as well, since the cam lobe profiles can be made different. After much criticism of the abruptness of power transition, Honda lowered the VTEC | 17,562 |
1402494 | Honda VFR800 | https://en.wikipedia.org/w/index.php?title=Honda%20VFR800 | Honda VFR800
activation rpm threshold to 6,400 rpm in 2006. The VTEC disengages two cylinder valves when the engine speed drops again below 6,100 rpm.
## 2014-Present VFR800F (RC79).
A facelifted VFR800 debuted at the 2013 EICMA show in Milan, Italy. The revised model features a new single sided exhaust system, akin to the fifth-generation one, lighter wheels, and additional mass-reduction, lowering the curb weight by . The new VFR also features traction control, a new instrument panel, and revised aerodynamic bodywork with LED lighting, though the engine and chassis remain largely unchanged from the previous sixth-generation model. Continued from the sixth-generation model is also the 2006 refined version | 17,563 |
1402494 | Honda VFR800 | https://en.wikipedia.org/w/index.php?title=Honda%20VFR800 | Honda VFR800
D lighting, though the engine and chassis remain largely unchanged from the previous sixth-generation model. Continued from the sixth-generation model is also the 2006 refined version of the VTEC system. The side-mounted heat exchangers were dropped in favour of a single front-mounted unit. The model is sold worldwide. In the US market, it is available in two versions: Standard and Deluxe. The Deluxe version adds ABS, traction control, grip heaters, center stand, and self-canceling turn signals. Outside the US, only the Deluxe version is sold.
# See also.
- Honda VF and VFR
- VFR1200F
- Honda VFR400
# External links.
- Honda VFR800 RC46 (1998-2001) and VTEC (2002-on) model information. | 17,564 |
1402497 | Ganswindt (crater) | https://en.wikipedia.org/w/index.php?title=Ganswindt%20(crater) | Ganswindt (crater)
Ganswindt (crater)
Ganswindt is a lunar impact crater that lies near the southern pole of the Moon's far side. It is attached to the southwestern exterior of the huge walled plain Schrödinger. Ganswindt partly overlies the smaller crater Idel'son to the south.
The rim of Gandswindt is roughly circular but somewhat irregular, particularly at the southern edge. Much of the interior floor is covered in uneven ridges, and there is a small crater in the southeastern section. Because sunlight enters the interior at a low angle, the northern part of the floor is almost always covered in shadow, concealing the terrain in that section of the crater.
The crater was named in honor of Hermann Ganswindt | 17,565 |
1402497 | Ganswindt (crater) | https://en.wikipedia.org/w/index.php?title=Ganswindt%20(crater) | Ganswindt (crater)
rn exterior of the huge walled plain Schrödinger. Ganswindt partly overlies the smaller crater Idel'son to the south.
The rim of Gandswindt is roughly circular but somewhat irregular, particularly at the southern edge. Much of the interior floor is covered in uneven ridges, and there is a small crater in the southeastern section. Because sunlight enters the interior at a low angle, the northern part of the floor is almost always covered in shadow, concealing the terrain in that section of the crater.
The crater was named in honor of Hermann Ganswindt (1856-1934), the aviation pioneer who first proposed reaction vehicles for space travel in 1881. He also proposed time as a fourth dimension. | 17,566 |
1402501 | Watteau (disambiguation) | https://en.wikipedia.org/w/index.php?title=Watteau%20(disambiguation) | Watteau (disambiguation)
Watteau (disambiguation)
Watteau is a French surname that may refer to:
# People with the surname.
- Jean-Antoine Watteau (1684–1721), French painter
- François-Louis-Joseph Watteau (1758–1823), French painter, son of Louis Joseph
- Louis Joseph Watteau (1731–1798), French painter, nephew of Jean-Antoine
# Other uses.
- Watteau dress, a stylistic school most influential in the design of gowns and their components
# See also.
- "Watteau in Venice", a novel
- Watto, a fictional character in the "Star Wars" universe | 17,567 |
1402500 | Tetsuya Takahashi | https://en.wikipedia.org/w/index.php?title=Tetsuya%20Takahashi | Tetsuya Takahashi
Tetsuya Takahashi
# Biography.
Born on November 18, 1966 in Shizuoka Prefecture in Japan. He began his career in video games in the 1980s working with Nihon Falcom.
## Squaresoft.
Takahashi worked on "Final Fantasy VI", including the design of the Magitek armor from the opening scene of the game. He also was the graphics director on "Chrono Trigger".
In 1995 he married his Squaresoft coworker Kaori Tanaka, better known by her pen name Soraya Saga.
## Xenogears.
Originally submitted as a potential plot for "Final Fantasy VII", it was made into its own project after being judged too dark and complicated for a fantasy game by others at Squaresoft.
## Monolith Soft.
While at Squaresoft, | 17,568 |
1402500 | Tetsuya Takahashi | https://en.wikipedia.org/w/index.php?title=Tetsuya%20Takahashi | Tetsuya Takahashi
Takahashi realized that the company intended to focus on the "Final Fantasy" series, and that sequels to the "Xenogears" series were becoming unlikely. He then decided to leave and start his own software development company. In October 1999 he left Squaresoft to start a new company, Monolith Soft, together with Hirohide Sugiura.
## Xenoblade Chronicles.
Following a meeting about the game "Soma Bringer", Takahashi imagined what a game would be like where the world was actually the body of a "giant god". Takahashi attempted a more "mature" writing style for the game, and said he expects to continue in the same vein in the future. The game references both Japanese and Western RPG styles, referring | 17,569 |
1402500 | Tetsuya Takahashi | https://en.wikipedia.org/w/index.php?title=Tetsuya%20Takahashi | Tetsuya Takahashi
to the western style in some cases "without thinking about it". In this way, the game is designed to appeal to fans of "text-based" JRPGs and western RPGs at the same time. Minor localizations were made for the American and European release, as well as bug fixes and game balancing. Originally Takahashi tried a more traditional turned based combat system, but he later incorporated a battle system where the protagonist can see into the future as a gameplay mechanic.
## Xenoblade Chronicles X.
Takahashi and Monolith Soft were revealed to be working on a new game for the Wii U in September 2012.
It was later revealed in the January 2013 Nintendo Direct under the tentative title X, and shown further | 17,570 |
1402500 | Tetsuya Takahashi | https://en.wikipedia.org/w/index.php?title=Tetsuya%20Takahashi | Tetsuya Takahashi
at E3 2013. For E3 2014, it was announced with the title "Xenoblade Chronicles X".
# Gameography.
- "" (1989): Art
- "Final Fantasy IV" (1991): Battle Graphics
- "Romancing SaGa" (1992): Field Graphics
- "Final Fantasy V" (1992): Field Graphics
- "Secret of Mana" (1993): Map Graphic Design
- "Final Fantasy VI" (1994): Graphic Director
- "Front Mission" (1995): Graphic Design
- "Chrono Trigger" (1995): Graphic Director
- "Seiken Densetsu 3" (1995): BG
- "Final Fantasy VII" (1997): Concept Art
- "Xenogears" (1998): Director, Scenario Writer
- "" (2002): Director, Scenario Writer
- "" (2004): Original Author
- "" (2004): Story Writer
- "Xenosaga I & II" (2006): Scenario Writer
- | 17,571 |
1402500 | Tetsuya Takahashi | https://en.wikipedia.org/w/index.php?title=Tetsuya%20Takahashi | Tetsuya Takahashi
BG
- "Final Fantasy VII" (1997): Concept Art
- "Xenogears" (1998): Director, Scenario Writer
- "" (2002): Director, Scenario Writer
- "" (2004): Original Author
- "" (2004): Story Writer
- "Xenosaga I & II" (2006): Scenario Writer
- "" (2006): Author, Music Coordinator, Supervisor of Scenario and Database
- "Soma Bringer" (2008): Producer, Game Designer
- "Xenoblade Chronicles" (2010): Concept, Executive Director, Scenario Writer
- "Xenoblade Chronicles X" (2015): Executive Director, Scenario Writer
- "Xenoblade Chronicles 2" (2017): Executive Director, Scenario Writer
- "" (2018): Executive director, Scenario Writer
# External links.
- "Tetsuya Takahashi" profile at MobyGames | 17,572 |
1402465 | 1940 Atlantic hurricane season | https://en.wikipedia.org/w/index.php?title=1940%20Atlantic%20hurricane%20season | 1940 Atlantic hurricane season
1940 Atlantic hurricane season
The 1940 Atlantic hurricane season was a generally average period of tropical cyclogenesis in 1940. Though the season had no official bounds, most tropical cyclone activity occurred during August and September. Throughout the year, fourteen tropical cyclones formed, of which nine reached tropical storm intensity; six were hurricanes. None of the hurricanes reached major hurricane intensity. Tropical cyclones that did not approach populated areas or shipping lanes, especially if they were relatively weak and of short duration, may have remained undetected. Because technologies such as satellite monitoring were not available until the 1960s, historical data on tropical | 17,573 |
1402465 | 1940 Atlantic hurricane season | https://en.wikipedia.org/w/index.php?title=1940%20Atlantic%20hurricane%20season | 1940 Atlantic hurricane season
cyclones from this period are often not reliable. As a result of a reanalysis project which analyzed the season in 2012, an additional hurricane was added to HURDAT. The year's first tropical storm formed on May 19 off the northern coast of Hispaniola. At the time, this was a rare occurrence, as only four other tropical disturbances were known to have formed prior during this period; since then, reanalysis of previous seasons has concluded that there were more than four tropical cyclones in May before 1940. The season's final system was a tropical disturbance situated in the Greater Antilles, which dissipated on November 8.
All three hurricanes in August brought flooding rainfall to areas of | 17,574 |
1402465 | 1940 Atlantic hurricane season | https://en.wikipedia.org/w/index.php?title=1940%20Atlantic%20hurricane%20season | 1940 Atlantic hurricane season
the United States. The first became the wettest tropical cyclone recorded in Louisiana history. The second hurricane impacted regions of the Southeastern United States, producing record precipitation and killing at least 52 people. Despite not making landfall, the third hurricane in August interacted with a stationary front over the Mid-Atlantic states, resulting in localized flooding and thus making the tropical cyclone the wettest in New Jersey history. This hurricane would also be the strongest in the hurricane season, with maximum sustained winds of 110 mph (175 km/h) and a minimum barometric pressure of 961 mbar (hPa; 28.39 inHg), making it a high-end Category 2 hurricane on the modern-day | 17,575 |
1402465 | 1940 Atlantic hurricane season | https://en.wikipedia.org/w/index.php?title=1940%20Atlantic%20hurricane%20season | 1940 Atlantic hurricane season
Saffir–Simpson hurricane wind scale. Activity decreased in September, though a damaging hurricane swept through areas of the Canadian Maritimes, resulting in large crop and infrastructural losses. Two tropical cyclones of at least tropical storm strength were recorded in October, though neither resulted in fatalities. Collectively, storms in the hurricane season caused 71 fatalities and $29.329 million in damages. The 1940 South Carolina hurricane, which swept through areas of the Southeastern United States in August, was the most damaging and deadly of the tropical cyclones.
# Systems.
## Tropical Storm One.
On May 18, a weak low-pressure area was detected south of Hispaniola. Moving northward, | 17,576 |
1402465 | 1940 Atlantic hurricane season | https://en.wikipedia.org/w/index.php?title=1940%20Atlantic%20hurricane%20season | 1940 Atlantic hurricane season
the low became sufficiently organized to be classified as a tropical storm at 1200 UTC on May 19, southeast of Turks Island. At the time, ship observations indicated that the disturbance had a well-defined cyclonic circulation, with the strongest winds situated in the northern semicircle of the cyclone. Continuing northward, the tropical storm gradually intensified and attained maximum sustained winds of 65 mph (100 km/h) by 0000 UTC on May 22. The Belgian ship "M.S. Lubrafol" recorded a peripheral barometric pressure of 996 mbar (hPa; 29.42 inHg); this was the lowest pressure measured in connection with the storm. The following day, the tropical storm temporarily curved towards the east-southeast | 17,577 |
1402465 | 1940 Atlantic hurricane season | https://en.wikipedia.org/w/index.php?title=1940%20Atlantic%20hurricane%20season | 1940 Atlantic hurricane season
before recurving back towards a northeast direction. At the same time, the storm expanded in size and began to transition into an extratropical cyclone. By 1200 UTC, the cyclone completed its extratropical transition, due to the entrainment of colder air. The remnant system persisted until 0600 UTC on May 27.
## Hurricane Two.
The 1940 Louisiana Hurricane
On August 3, an extratropical cyclone developed into a tropical depression off the west coast of Florida. Initially a weak disturbance, it moved generally westward, slowly gaining in intensity. Early on August 4, the depression attained tropical storm intensity. Ships in the vicinity of the storm reported a much stronger tropical cyclone | 17,578 |
1402465 | 1940 Atlantic hurricane season | https://en.wikipedia.org/w/index.php?title=1940%20Atlantic%20hurricane%20season | 1940 Atlantic hurricane season
than initially suggested. After reaching hurricane strength on August 5 south of the Mississippi River Delta, the storm strengthened further into a modern-day Category 2 hurricane, with maximum sustained winds of 100 mph (155 km/h) and a minimum barometric pressure of 972 mbar (hPa; 28.71 inHg) at 0600 UTC on August 7. The hurricane moved ashore near Sabine Pass, Texas later that day at peak strength. Once inland, the storm executed a sharp curve to the north and quickly weakened, degenerating into a tropical storm on August 8 before dissipating over Arkansas on August 10.
Reports of a potentially destructive hurricane near the United States Gulf Coast forced thousands of residents in low-lying | 17,579 |
1402465 | 1940 Atlantic hurricane season | https://en.wikipedia.org/w/index.php?title=1940%20Atlantic%20hurricane%20season | 1940 Atlantic hurricane season
areas to evacuate prior to the storm moving inland. Offshore, the hurricane generated rough seas and a strong storm surge, peaking at 6.4 ft (1.95 m) on the western edge of Lake Pontchartrain. The anomalously high tides flooded many of Louisiana's outlying islands, inundating resorts. Strong winds caused moderate infrastructural damage, primarily in Texas, though its impact was mainly to communication networks along the U.S. Gulf Coast which were disrupted by the winds. However, much of the property and crop damage wrought by the hurricane was due to the torrential rainfall it produced in low-lying areas, setting off record floods. Rainfall peaked at 37.5 in (953 mm) in Miller Island off Louisiana, | 17,580 |
1402465 | 1940 Atlantic hurricane season | https://en.wikipedia.org/w/index.php?title=1940%20Atlantic%20hurricane%20season | 1940 Atlantic hurricane season
making it the wettest tropical cyclone in state history. Nineteen official weather stations in both Texas and Louisiana observed record 24-hour rainfall totals for the month of August as a result of the slow-moving hurricane. Property, livestock, and crops – especially cotton, corn, and pecan crops – were heavily damaged. Entire ecosystems were also altered by the rainfall. Overall, the storm caused $10.75 million in damages and seven fatalities.
## Hurricane Three.
The 1940 South Carolina Hurricane
A storm of potentially Cape Verde origin was detected in the Virgin Islands at 1800 UTC on August 5. Initially moving westward, the tropical storm gradually gained in intensity before making a | 17,581 |
1402465 | 1940 Atlantic hurricane season | https://en.wikipedia.org/w/index.php?title=1940%20Atlantic%20hurricane%20season | 1940 Atlantic hurricane season
sharp curve towards the north on August 8. The storm continued in a northerly motion before a second curvature brought it in a generally westward direction on August 9. Shortly after, the tropical storm reached hurricane intensity as a modern-day Category 1 hurricane. The hurricane eventually made landfall at peak intensity on Hilton Head Island, South Carolina at 2030 UTC on September 21. At the time, the storm had maximum sustained winds of 100 mph (155 km/h) and a minimum central pressure of 972 mbar (hPa; 28.71 inHg), equivalent to a modern-day Category 2 hurricane. Once inland, the tropical cyclone gradually weakened, and recurved northeastward before dissipating over the Appalachian Mountains | 17,582 |
1402465 | 1940 Atlantic hurricane season | https://en.wikipedia.org/w/index.php?title=1940%20Atlantic%20hurricane%20season | 1940 Atlantic hurricane season
on August 14.
The hurricane dropped torrential rainfall over the Southeast United States, causing unprecedented devastation in the region. The storm was considered the worst to impact in the region in at least 29 years. Precipitation peaked at 20.65 in (525 mm) in Idlewild, North Carolina. The heavy rainfall caused streams to greatly exceed their respective flood stages, damaging waterfront property. Many of the deaths occurred in North Carolina, where 30 people died. Transportation was disrupted as a result of the debris scattered by the wind and rain. In Caldwell County alone, 90 percent of bridges were swept away. Overall, the storm caused 50 fatalities and $13 million in damages.
## Hurricane | 17,583 |
1402465 | 1940 Atlantic hurricane season | https://en.wikipedia.org/w/index.php?title=1940%20Atlantic%20hurricane%20season | 1940 Atlantic hurricane season
Four.
On August 26, a low-pressure area in the open Atlantic Ocean became sufficiently organized to be classified as a tropical cyclone. Moving slowly in a general west-northwest motion, the disturbance intensified, reaching tropical storm strength on August 28 and subsequently hurricane intensity on August 30. The hurricane passed within 85 mi (135 km) of Cape Hatteras before recurving towards the northeast. However, the hurricane continued to intensify, and reached peak intensity as a modern-day Category 2 hurricane with maximum sustained winds of 110 mph (175 km/h) and a minimum barometric pressure of 961 mbar (hPa; 28.38 inHg), though these statistical peaks were achieved at different times | 17,584 |
1402465 | 1940 Atlantic hurricane season | https://en.wikipedia.org/w/index.php?title=1940%20Atlantic%20hurricane%20season | 1940 Atlantic hurricane season
on September 2. Afterwards, the tropical cyclone began a weakening trend as it proceeded northward, and had degenerated into a tropical storm by the time it made its first landfall on Nova Scotia later that day. The storm transitioned into an extratropical cyclone the next day while making another landfall on New Brunswick. The extratropical remnants persisted into Quebec before merging with a larger extratropical system late on September 3.
Despite not making landfall on the United States, the hurricane caused widespread damage. Extensive precautionary measures were undertaken across the coast, particularly in New England. The heightened precautions were due in part to fears that effects from | 17,585 |
1402465 | 1940 Atlantic hurricane season | https://en.wikipedia.org/w/index.php?title=1940%20Atlantic%20hurricane%20season | 1940 Atlantic hurricane season
the storm would be similar to that of a devastating hurricane which struck the region two years prior. Most of the damage associated with the hurricane occurred in New Jersey, where the combination of moisture from the hurricane and a stationary front produced record rainfall, peaking at 24 in (610 mm) in the town of Ewan. This would make the storm the wettest in state history. The resultant floods damaged infrastructure, mostly to road networks. Damage in the state amounted to $4 million. Further north in New England, strong winds were reported, though damage remained minimal. Although the storm made two landfalls in Atlantic Canada, damage there too was minimal, and was limited to several | 17,586 |
1402465 | 1940 Atlantic hurricane season | https://en.wikipedia.org/w/index.php?title=1940%20Atlantic%20hurricane%20season | 1940 Atlantic hurricane season
boating incidents caused by strong waves. Overall, the hurricane caused $4.05 million in damage, primarily due to flooding in New Jersey, and seven fatalities.
## Hurricane Five.
A tropical depression was first detected east of the Lesser Antilles on September 7, though at the time weather observations in the area were sparse. The disturbance gradually intensified throughout much of its early formative stages, attaining tropical storm strength on September 10; further strengthening into a hurricane north of Puerto Rico occurred two days later. Shortly thereafter, the hurricane recurved northward, and reached peak intensity the following day as a modern-day Category 2 hurricane with maximum | 17,587 |
1402465 | 1940 Atlantic hurricane season | https://en.wikipedia.org/w/index.php?title=1940%20Atlantic%20hurricane%20season | 1940 Atlantic hurricane season
sustained winds of 100 mph (160 km/h) and a minimum barometric pressure of at least 988 mbar (hPa; 29.18 inHg). The cyclone steadily weakened thereafter before making landfall on Nova Scotia on September 17 with winds of 85 mph (135 km/h). Moving into the Gulf of Saint Lawrence later that day, the storm transitioned into an extratropical cyclone. The remnant system curved eastward and passed over Newfoundland before dissipating over the Atlantic on September 19.
While off of the United States East Coast, the hurricane caused numerous shipping incidents, most notably the stranding of the Swedish freighter "Laponia" off of Cape Hatteras, North Carolina on September 16. Two other boat incidents | 17,588 |
1402465 | 1940 Atlantic hurricane season | https://en.wikipedia.org/w/index.php?title=1940%20Atlantic%20hurricane%20season | 1940 Atlantic hurricane season
resulted in two deaths. The hurricane also brought strong winds of tropical storm-force and snow over areas of New England. In Atlantic Canada, a strong storm surge peaking at 4 ft (1.3 m) above average sunk or damaged several ships and inundated cities. In New Brunswick, the waves hurt the lobster fishing industry. In Nova Scotia, strong winds disrupted telecommunication and power services. The winds also severely damaged crops. Roughly half of apple production in Annapolis Valley was lost during the storm, resulting in around $1.49 million in economic losses. Strong winds in New Brunswick caused moderate to severe infrastructural damage, and additional damages to crops occurred there. Overall, | 17,589 |
1402465 | 1940 Atlantic hurricane season | https://en.wikipedia.org/w/index.php?title=1940%20Atlantic%20hurricane%20season | 1940 Atlantic hurricane season
the hurricane caused three fatalities, with two off of the United States and one in New Brunswick.
## Tropical Storm Six.
A westward moving tropical depression developed in the southwestern Caribbean Sea just west of Bluefields, Nicaragua at 1200 UTC on September 18. The following day, the depression intensified into a tropical storm at 0600 UTC. The tropical storm made landfall on the Mosquito Coast of Nicaragua at 1400 UTC, with winds of 40 mph (65 km/h). The cyclone weakened to a tropical depression over land, but reintensified back to tropical storm strength upon entry into the Gulf of Honduras on September 20. The cyclone's northwest motion caused it to make a second landfall near the | 17,590 |
1402465 | 1940 Atlantic hurricane season | https://en.wikipedia.org/w/index.php?title=1940%20Atlantic%20hurricane%20season | 1940 Atlantic hurricane season
border of Mexico and British Honduras at 0300 UTC on September 21 as a slightly stronger system with winds of 50 mph (85 km/h); this would be the storm's peak intensity. Over the Yucatán Peninsula, the tropical storm re-weakened, but later intensified once again once it reached the Gulf of Mexico. In the Gulf, the storm made a gradual curve northward, before making a final landfall near Lafayette, Louisiana at 0900 UTC on September 24 with winds of 45 mph (75 km/h) and a minimum barometric pressure of 1002 mbar (hPa; 29.59 inHg). Once inland, the tropical cyclone curved eastward and weakened before dissipating the next day, after becoming absorbed by a frontal boundary.
Upon making landfall, | 17,591 |
1402465 | 1940 Atlantic hurricane season | https://en.wikipedia.org/w/index.php?title=1940%20Atlantic%20hurricane%20season | 1940 Atlantic hurricane season
the tropical storm produced strong winds over a wide area. The strongest winds were reported by a station in San Antonio, Texas, which reported 40 mph (65 km/h) winds, far removed from the storm's center; these strong winds were likely due to squalls. Heavy rainfall was also reported, though the rains mainly occurred to the east of the passing tropical cyclone. Precipitation peaked at 10 in (254 mm) in Ville Platte, Louisiana. The tropical storm produced three tornadoes over the Southern United States which collectively caused $39,000 in damage and caused two fatalities. Two of the tornadoes formed in Mississippi while one formed in Louisiana. Several other people were also injured by the tornadoes.
## | 17,592 |
1402465 | 1940 Atlantic hurricane season | https://en.wikipedia.org/w/index.php?title=1940%20Atlantic%20hurricane%20season | 1940 Atlantic hurricane season
Hurricane Seven.
In late September, a tropical wave persisted in the northeastern Atlantic Ocean. The low-pressure area later became sufficiently organized to be classified as a tropical storm at 0000 UTC on September 22. The disturbance quickly organized after tropical cyclogenesis, and reached a strength equivalent to a modern-day Category 1 hurricane strength at 1800 UTC later that day. The American steamship "Otho" encountered the system that day, and reported gale-force winds in conjunction with a peripheral barometric pressure of 996 mbar (hPa; 29.42 inHg). The tropical cyclone continued to the east-northeast, where it gradually intensified. At 1200 UTC on September 23, the hurricane | 17,593 |
1402465 | 1940 Atlantic hurricane season | https://en.wikipedia.org/w/index.php?title=1940%20Atlantic%20hurricane%20season | 1940 Atlantic hurricane season
attained modern-day Category 2 hurricane intensity with winds of 100 mbar (155 km/h); a peak which would be maintained for at least the following 12 hours. A second steamship, the "Lobito", reported hurricane-force winds along with a minimum pressure of 977 mbar (hPa; 28.85 inHg); this would be the lowest pressure measured associated with the tropical cyclone. After reaching peak intensity, the hurricane began a weakening trend, and degenerated to a Category 1 hurricane at 0600 UTC as it passed over the Azores. The following day, the hurricane recurved westward, where it weakened before transitioning into an extratropical cyclone on September 28. This remnant system subsequently dissipated.
As | 17,594 |
1402465 | 1940 Atlantic hurricane season | https://en.wikipedia.org/w/index.php?title=1940%20Atlantic%20hurricane%20season | 1940 Atlantic hurricane season
the hurricane passed over the Azores, several weather stations reported low barometric pressures, with the lowest being a measurement of 984 mbar (hPa; 29.06 inHg) on Terceira Island at 0600 UTC on September 25. As a result of the impending storm, several Pan Am Clipper flights to the archipelago were suspended for three consecutive days. The maximum reported gust in the Azores was an observation of 65 mph (100 km/h) on September 25. As a result of moving slowly over the islands, torrential rainfall was also reported. At Angra do Heroísmo, 13.11 in (333 mm) of precipitation was reported in a four-day, accounting for a third of the station's yearly average rainfall. Strong storm surge was reported | 17,595 |
1402465 | 1940 Atlantic hurricane season | https://en.wikipedia.org/w/index.php?title=1940%20Atlantic%20hurricane%20season | 1940 Atlantic hurricane season
at the same location. The waves swept boats away from the coasts of islands. Further inland, there was extensive damage to homes and crops, though no people died. Despite evidence that the system had distinct tropical characteristics, it was not operationally added to HURDAT.
## Hurricane Eight.
On October 19, a low-pressure area moved into the southwestern Caribbean Sea. The area of disturbed weather quickly became well-organized, and was analyzed to have become a tropical depression at 0000 UTC on October 20. Initially, the tropical cyclone moved very slowly towards the west and then the northwest. Shortly after formation, the disturbance intensified into a tropical storm at 1800 UTC later | 17,596 |
1402465 | 1940 Atlantic hurricane season | https://en.wikipedia.org/w/index.php?title=1940%20Atlantic%20hurricane%20season | 1940 Atlantic hurricane season
that day. The "S.S. Cristobal" provided the first indications of a tropical cyclone in the region, after reporting strong gusts and low pressures north of the Panama Canal Zone during that evening. Continuing to intensify, the storm reached hurricane intensity at 0600 UTC on October 22. Several vessels in the storm's vicinity reported strong gusts and rough seas generated by the storm. Later that day at 1200 UTC, the ship "S.S. Castilla" reported a minimum pressure of 983 mbar (hPa; 29.03 inHg) near the periphery of the storm. Based on this observation, the hurricane was estimated to have reached intensity at the same time with winds of 80 mph (130 km/h). The hurricane subsequently curved west | 17,597 |
1402465 | 1940 Atlantic hurricane season | https://en.wikipedia.org/w/index.php?title=1940%20Atlantic%20hurricane%20season | 1940 Atlantic hurricane season
and then southwest, before making its only landfall in northern Nicaragua at 1900 UTC on October 23 at peak intensity. Once inland, the tropical cyclone rapidly weakened over mountainous terrain, and dissipated at 1200 UTC the following day. Reports of damage were limited, though a report stated that considerable damage had occurred where the hurricane made landfall.
## Tropical Storm Nine.
On October 23, an open trough was centered north of Hispaniola near the Turks and Caicos islands. At 0000 UTC the following day, the area of disturbed weather became organized and was analyzed to have become a tropical storm southeast of Inagua, based on nearby vessel reports. Initially, the storm drifted | 17,598 |
1402465 | 1940 Atlantic hurricane season | https://en.wikipedia.org/w/index.php?title=1940%20Atlantic%20hurricane%20season | 1940 Atlantic hurricane season
northward, but later began to accelerate towards the northeast after a roughly 12-hour period. At 0600 UTC on October 25, the disturbance slightly gained in intensity to attain maximum wind speeds of 45 mph (75 km/h); these would be the strongest winds associated with the storm as a fully tropical cyclone. A reanalysis of the system indicated that due to a lack of definite tropical features, the storm may have had been a subtropical cyclone. On October 26, the system became increasingly asymmetric and had developed frontal boundaries, allowing for it to be classified as an extratropical cyclone at 0600 UTC that day. Once transitioning into an extratropical system, the storm continued to intensified | 17,599 |
Subsets and Splits
No community queries yet
The top public SQL queries from the community will appear here once available.