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There definitely seems to be a supercell-type storm near the northern GA coast, though it appears to have been spawned by a somewhat larger-scale (larger than supercell scale, but small-scale in the grand scheme of things) circulation. Convection continues to increase in the northern Caribbean. Westerly shear seems to have given way to northeasterly shear in that area, though the overall shear seems less than in the last couple of days. No signs of anything developing at the surface there. |