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As the 5 p.m disco had mentioned, a 10 C cold pool had developed over LA. This would in turn deepen the ULL dropping down, and bring about the presence of a deep SEasterly steering flow. This i believe is being reflected in some models. The nighttime presistent westward movement maybe has something to do with problems with adibiatic heating of the 850 temperatures, which would affect the Upper level features differently; that's my take. |