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.

Switch images by moving your mouse pointer over numbered buttons...

slide 7


Slide 7