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http://www.ssd.noaa.gov/PS/TROP/DATA/RT/watl-ir4-loop.html this loop may illustrate what steve mentioned. Notice the convection aroun dthe Keyes and points further south being 'pushed' north with what seems to be part of this storms environment or a weakness to the ridge or a combo of the two. Meaning the outflow is pushing convecrtion north and there is not enough ridge to block that stray convection or divert it. I am probably way off so bare with me! Still in kindergarten here with regards to my weather schoolage : |