#3 Postby vbhoutex » Sat Jun 04, 2005 8:01 am
From what I see on both radars it is the convection associated with the trough and broad low circulating around the low, not a mid level circulation. The convection on the west side does not turn back to the E at any point I see. That would be needed for true circulation. That low and the trough associated with it stretch all the way from the panhandle to the NW Carribean.
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