#19 Postby Hyperstorm » Thu Jul 21, 2005 8:34 am
The wave is VERY big as you've mentioned and that will likely cause it to be slow to develop. Once the low moves west into the Caribbean, it should start generating some convection, but since it is drawing strong subsidence from the north, developmental chances in the central and eastern Atlantic are basically zero.
Since it is a low of such HIGH-amplitude, it is drawing huge amounts of dry/cool air from the north ahead of it and heavy amounts of moisture behind it. What's impressive about it is that these types of waves serve as a barrier from the dry air for the waves that come right behind them.
0 likes