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Hurricane Season
2003 Statistical normals of storm frequencies for the North Atlantic
hurricane season, based on the 1950-2000 average, are 10 named storms, 6
of which become hurricanes, and 2 of those typically become intense
hurricanes. Last year in 2002, there were 12 named storms, 4 of which
became hurricanes, and 2 of those became intense hurricanes. Only one of
the hurricanes, Lili, made landfall while still a hurricane.
Although the
number of named storms exceeded the normal seasonal total, the El Ni�o
event that was then present, and still is, kept the number of hurricanes
to below normal levels. In spite of this, some portion of the U.S. East
and Gulf coasts from the Lower Texas coast to Cape Hatteras was impacted
by these storms. This is likely to be the case again this year.
El Ni�o is an
occurrence of warmer than normal sea surface temperatures in the
equatorial Pacific Ocean. This year the warmer  Figure 1. Sea
surface temperature anomaly chart from 0000UTC 8 March 2003; courtesy of
Unisys. Shades of green and yellow represent warmer than normal water;
shades of blue are cooler than normal water.
waters extend
from Indonesia eastward across the Central Pacific but they are now less
than 2� C warmer than usual. In the eastern Tropical Pacific, the sea
surface temperatures (SST's) are near or slightly cooler than normal at
and south of the equator (see figure 1). This El Ni�o event is different
from the previous one (1997-1998), during which the Tropical Pacific
waters were much warmer, primarily in the central and eastern protions of
the equatorial waters (see figure 2).
 Figure 2. Sea surface temperature anomaly
chart from 1200UTC 28 April 1998; courtesy of Unisys. Shades of green,
yellow, orange and red represent warmer than normal water; shades of blue
and purple are cooler than normal water.
We must
keep in mind the fact that these two El Ni�o episodes are different when
looking to the upcoming hurricane season. Additionally, the current El
Ni�o appears to be weakening and sea surface temperatures may become near
normal in the equatorial region of the Pacific Ocean by the first few
months of hurricane season.
The
influence on this year�s El Ni�o on the summer time high level wind
pattern across the North Atlantic Ocean basin is forecast to be in the
form of upper level high pressure areas that move slowly from west to east
across the subtropical latitudes (20-35 degrees north latitude) separated
by low pressure troughs. These troughs of weak upper air low pressure
should drop into the tropical latitudes (0-20 north latitude) at various
times and disrupt the development of some tropical disturbances.
Additionally, it is quite likely that a few of the named storms will
develop out of mid-latitude cyclones located east of Bermuda that form
tropical characteristics but remain inconsequential due to their tracks
staying well away from land and out of major shipping lanes.
As a
result, we expect an above normal number of named storms this year. Near
or slightly less than the normal number of storms are forecast to reach
hurricane strength. Of those, 3 are expected to become intense. Most of
these storms should form in the western North Atlantic region with fewer
forming farther to the east in the general vicinity of the Cape Verde
Islands. Further weakening of El Ni�o during the remainder of the year
would cause the latter half of this year�s hurricane season to be more
active than the earlier half.
2003 Hurricane Season Forecast
|
Normal |
Forecast |
| Total number of named storms |
10 |
12-14 |
| Named storms becoming hurricanes |
6 |
6 |
| Hurricanes becoming intense |
3 |
3 |
Dr.
William Gray of Colorado State University issued his forecast for the 2003
Hurricane Season early in April. His assessment of the future of the
present El Ni�o event agrees with ours in that it is expected to weaken to
a neutral state during the summer months. Our forecast differs from his
very little this year. The threshold between tropical storm and hurricane
status is between 70-75 mph and it is possible for a few more of the
tropical storms to cross the line to minimal hurricane status for a brief
period of time. The forecast for the probability of where we expect these
to form and their likely movement from those areas is indicated in Figure
3.
 Figure 3.
Probability of Development and Movement of Tropical Cyclones (depressions,
storms and hurricanes) � WWT Forecast for the 2003 hurricane
season.
http://www.wilkensweather.com
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