850 mb heights temperature and frontogenesis
Notes:
At 850 mb, the flow was characterized by strong warm advection through the period. A maximum of frontogenesis can be seen over western New York and northeast Pennsylvania early on the 30th. The frontogenesis weakened, then strengthened in a small area over northeast Pennsylvania by late on the 30th.The strengthening occurred as the low center was become increasingly intense and compact along the New Jersey coast.
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Slide 7