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1995 PRELIMINARY
REPORTS |
a. Synoptic HistorySatellite images indicate that an area of cloudiness, associated
with a tropical wave that left western Africa on 9 August, propagated
westward across the tropical Atlantic from the 9th to the 15th of August.
Even though convection increased when the wave neared the Lesser Antilles
on the 15th, there were no large surface pressure falls noted in those
islands. When the wave moved over the eastern and central Caribbean Sea,
rawinsonde data from San Juan and Santo Domingo revealed that the system
was fairly strong at mid- to lower-tropospheric levels, as evidenced by
35- to 46-mph wind reports east of the wave axis
at 850 and 700 mb. By the 19th, satellite pictures and surface data gave some
evidence of a low-level circulation centered near 18N 75W at 1200 UTC.
No further development occurred during the next couple of days as the
system moved west-northwestward to northwestward, interacting with the
mountainous land mass of eastern Cuba. On the 22nd, cloudiness and convection
became better organized near the western Bahamas, and surface reports
indicate that a tropical depression formed from this system a short distance
southwest of Andros Island at 1800 UTC 22 August. Upper-level winds were
partially favorable for development, since anticylonic outflow prevailed
over the eastern half of the depression while outflow was inhibited to
the west and northwest. As the depression moved north-northwestward toward southeast
Florida, slow strengthening took place. Based on measurements from a NOAA
plane, it is estimated that the system strengthened to a tropical storm
around 1200 UTC on the 23rd. Tropical Storm Jerry made landfall later
that same day near Jupiter, Florida as a 40-mph storm. Jerry moved northwest to west-northwest
across the Florida peninsula, weakening back to a tropical depression
by 1800 UTC on the 24th while nearing the upper west coast of Florida.
The forward motion slowed, and after the center drifted a short distance
out over the waters of the Gulf of Mexico, Jerry turned toward the north
and moved inland again over northern Florida and across the Georgia/Florida
border on 25 August. The weak depression moved slowly northward to north-northwestward
over Georgia on the 26th and 27th. Later on the 27th, Jerry turned eastward
toward South Carolina. By 0000 UTC on the 28th, the circulation of Jerry
became elongated in a northeast-southwest oriented trough, and six hours
later it was impossible to distinguish a circulation center. However,
the trough persisted near the Carolinas during the next couple of days
and two discrete low pressure centers appeared. The first moved eastward
from the coast of North Carolina into the Atlantic without significant
development. The second became evident just offshore of the Georgia/South
Carolina border early on the 29th. This weak surface low moved southward
and southwestward, across the Florida peninsula on 30-31 August, and died
a slow death over the southeast Gulf of Mexico during the first few days
of September. There was, and still is, confusion concerning which, if
any, of these two lows was derived from the original circulation of Jerry.
b. Meteorological Statistics
|
Date/Time (UTC) |
Position | Pressure (mb) |
Wind Speed (mph) |
Stage | |
---|---|---|---|---|---|
Lat. (°N) | Lon. (°W) | ||||
24/1200 | 28.4 | 81.8 | 1004 | 40 | Tropical Storm |
Minimum
Pressure For Tropical Storm Jerry
22 - 28 August, 1995
Date/Time (UTC) |
Position | Pressure (mb) |
Wind Speed (mph) |
Stage | |
---|---|---|---|---|---|
Lat. (°N) | Lon. (°W) | ||||
24/1800 | 28.8 | 82.6 | 1002 | 35 | Tropical Storm |
Landfall
for Tropical Storm Jerry
22 - 28 August, 1995
Date/Time (UTC) |
Pressure (mb) |
Wind Speed (mph) |
Stage | Landfall |
---|---|---|---|---|
23/1800 | 1006 | 40 | Tropical Storm | Jupiter, Florida |