#37 Postby weatherwindow » Sun Jun 12, 2005 8:09 pm
good insight, rainstorm.....tropical development in the western carib is benefitting from low level sw inflow from the eastern pacific and anomolously low pressures via the monsoon trough....as for the disturbance in the central carib, most of the models are depicting a rapid weakening of the ridge to its north. ...none of them are suggesting serious westward motion. with varying speed, all are taking any low immediately northeast over the bahamas. i dont see this as a potential threat to the GOM..........rich
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