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06/12/07
The second week of June is passing without the formation of a third
tropical cyclone for the season, just barely. In the two weeks past
since our last Hurricane Watch only one system has shown any
possibilities of cyclonic development, TD3E. But today it became
evident that the tropical depression was moving into cooler water and
more stable air, all but precluding further development.
The first week of June saw the arrival of the first
Tropical Wave to make it's way across the Atlantic, South America then
into the Eastern Pacific basin. At the time of the writing of writing
of this article there are three tropical waves in our basin - none of
them likely to form a tropical cyclone in the imminent future. The
Pacific basin has remained fairly dry following the formation of TD3E,
providing little unstable air for these tropical waves to stimulate.
Tropical Depression 3E had showed some potential for
cyclonic development but never posed any threat to land. The storm
formed about 440 miles SW of Manzanillo and moved WNW over the next
24hrs before encountering colder water and dryer and more stable air.
At the time of this article the system was about 450 miles SW of Cabo
San Lucas and moving WNW. Forecasts call for the storm to dissipate by
Wednesday.
So, why can we rest virtually assured that these early
season storms pose no threat to Baja? There are a wide variety of
factors that influence the formation and path of the storms. Weather
Science has yet to define all the aspects of forecasting hurricanes,
which becomes evident when professional forecasters miss the mark.
When we look at the various computer models developed by Government
agencies from different nationals and private industry we see there is
no clear consensus. The familiar plot from the National
Hurricane
Center rarely represents any of the computer models, but is
rather an average of the projected storm tracks.
Last season, when Hurricane John approached Baja Sur
for landfall on September 1, one model called for John to bank to the
right and make landfall on the mainland side. Another model call for
John to get caught up in a westward flow and pass harmlessly south of
Cabo San Lucas. Yet another called for John to move right up the
middle of the Sea. A scant 48hrs before the storm made landfall on
East Cape only one of the computer models was forecasting that
outcome. However, the NHC averaging model had begun predicting East
Cape Landfall about 6hrs before
More below...
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