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Yesterday the NHC referenced the low in the Carribean as a broad surface low with a pressure of 1007mb, actually lower than the Atlantic low (1010mb)...what I see going on in the Carribean is what has been going on since last Thursday...there is a broad surface low, but there is an upper feature overriding it and the convection is in response to the upper feature (dry air)...not a tropical system at all...still a lot of shear west to east... |