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1988 PRELIMINARY
REPORTS
Tropical Storm Alberto (TS) |
a. Synoptic HistoryTropical Storm Isaac can be traced back to a weak disturbance
that was near the west coast of Africa on 23 September. This low latitude
disturbance quickly merged with the intertropical convergence zone and
moved westward in an undistinguished manner. On the 27th, satellite imagery
showed a concentration and organization of convective activity in the
mid Atlantic. On the 29th, the system was identified as Tropical Depression
Sixteen while centered about 900 nautical miles east southeast of of Barbados,
based on an interpretation of satellite imagery. Depression Sixteen moved westward at 16 mph. On the 30th,
it shifted two degrees of latitude northward, possibly as a result of
the formation of a new center. It then continued continued westward, crossing
through the southern Lesser Antilles and into the southeastern Caribbean
on 1 and 2 October. Also, its forward speed increased to 21 mph during
this period. b. Meteorological StatisticsThe maximum 1-minute surface wind speed and the minimum surface
pressure curves as a function of time are shown in Figures 2 and 3, along
with the observations on which these are based. The short time that Isaac's
surface winds were 39 mph or higher is reflected in the sharpness of the
peak curve. The maximum 1-minute surface wind speed during Isaac's existance
is estimated to be 46 mph, which is 80% of the highest aircraft flight
level wind. The National Hurricane Center (NHC) satellite wind speed estimates
appear to have a slight positive bias. That is, the center passed about
60 nautical miles south of Barbados at the time of the 0600 UTC. NHC satellite
wind speed of 52 mph and barbados' surface winds were only 12 mph at the
time.
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Date/Time (UTC) |
Position | Pressure (mb) |
Wind Speed (mph) |
Stage | |
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Lat. (°N) | Lon. (°W) | ||||
01/0000 | 11.8 | 57.7 | 1005 | 45 | Tropical Storm |