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TP Zcusum
SNB TP
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TP Zcusum
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TP Zcusum
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Figure 3.21: TOC Zcusum charts for water quality segments in Biscayne Bay
Chlorophyll a
Chlorophyll a followed a similar pattern in all segments, except at MBS and CS.
As for TP, hurricanes Katrina, Rita and Wilma triggered unprecedented CHLa blooms in
MBS and CS, which distorts the time-series pattern. As shown above, when posthurricane data is discarded, all segments display a common pattern (Fig 3.22). This
pattern is characterized by a below-average tendency until 1999 when Hurricane Irene
impacted South Florida. Irene produced heavy rainfall across southeastern Florida,
peaking at 17.45 inches at Boynton Beach and 10-15 inches in Miami Metropolitan
area. Most heavy rain from Irene was concentrated over Biscayne Bay watershed (Fig
3.23), which coupled with large water releases from canals to avoid flooding of Miami,
contributed to the development of a large algal bloom in the Bay. After ten months
(early-mid 2000) CHLa concentrations had returned to mostly below average levels in
SCI, SCM, SCO, SNB and NNB (similar Zcusum slope as before impact). After mid2003 an above average trend set in lasting until 2007, when a new decline began. On
the other hand, and underscoring the combined natural and anthropogenic impacts, the
2005 bloom persisted for four years in MBS.
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TOC Zcusum
MBS TOC
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