Let's consider how upper air flow affects development of weather systems. My article illustrating a detailed surface analysis (not here yet) concerned a small storm system most typical of those in North America. This one features the more unusual (and probably interesting) case of a large snowstorm, which dropped 2 feet at most favorable locations near the southern west shore of Lake Michigan and more than a foot over much of the Great Lakes region. This article involves detailed analyses of 500 mb and 850 mb charts, precipitation type and its relation with predictive weather parameters, and snowfall maps.
Surface chart : 1 January 1999, 00 UTC
Surface chart : 1 January 1999, 12 UTC
Surface chart : 2 January 1999, 00 UTC
Surface chart : 2 January 1999, 12 UTC
Surface chart : 3 January 1999, 00 UTC
Surface chart : 3 January 1999, 12 UTC
Surface chart : 4 January 1999, 00 UTC
that such development occurred in a region of large temperature gradient (temperature shown at upper left of each station plot), and the associated upper air situation - particularly at 500 mb (middle atmosphere) the trof aloft which develops in the flow over the NW U.S. and strengthens while moving southeastward, and the cold closed Low which subsequently formed over the middle U.S.
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Text is copyright of Joseph Bartlo, though may be used with proper crediting.