#138 Postby Hyperstorm » Tue Jul 31, 2007 8:39 am
Understand that I'm not saying that the system won't develop at all during its lifetime. It justs doesn't seem like it is imminent or likely.
Look at the structure of the system (NOT the convection), and you'll see an ill (box-like) structure. There is definitely something that is coming off of South America...I call it mid-level shear. That is very common in the region and is usually associated with the outflows of the thunderstorms that develop over land and travel northward. That's likely one of the reasons why systems do fail to develop a good center of circulation when in close contact to the South-American continent. Another factor that tells me any development is in "status quo" at this time, is the lack of convection during what is supposed to be the time when convection is supposed to be continually expanding. Remember, that we usually see a decline of convection during the afternoon and early evening and NOT during the morning hours. Of course, that would happen when there is a good structure with the system...which brings me back to my original point.
It would not be surprising to see it persist (as a wave) until it reaches the central and western Caribbean, where its potential for development could skyrocket depending on environmental conditions.
In any case, it will likely bring some very squally weather to the islands over the next 3 days...
Last edited by
Hyperstorm on Tue Jul 31, 2007 8:40 am, edited 1 time in total.
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