850-700 frontogenesis, 700-500 lapse rate and the Trowal
Notes:
Frontogenesis developed on the southwest side of the trowal, as the trowal strengthened and developed westward from the western Atlantic toward upstate New York. Theta-e lapse rates of 1 degree C or less developed in the trowal over central New England between 00z and 06z on the 26th. Otherwise, lapse rates within the trowal were mainly 2 to 4 degrees C.|
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Valid Thu 0600 UTC 25-Feb-2010 Valid Thu 1200 UTC 25-Feb-2010 Valid Thu 1800 UTC 25-Feb-2010 Valid Fri 0000 UTC 26-Feb-2010 Valid Fri 0600 UTC 26-Feb-2010 Valid Fri 1200 UTC 26-Feb-2010 |
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Slide 15