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900 mb temperature and 1000-850 mb frontogenesis


900 mb temperature and 1000-850 mb frontogenesis

Notes:

The effect of the Great Lakes on the temperature field and resultant frontogenesis field is shown on the next few slides. Warm plumes developed over both lake Huron and lake Ontario, which resulted in the development of lake-induced frontal zones downwind of both lakes.


Slide 12