I saw the same thing on the GHCC satellite site. Lower clouds are moving in a cyclonic motion. While the upper level high, thin cirrus are moving anticyclonic. This would be somewhat favorable for development. I do think there is a low pressure trough line that extends to the south of the disturbance. Based on converging winds. This could be the lower tropical wave. I'm not an expert by any means.
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Re: Wave in the Caribbean, Part II
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