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Great Salt Lake effect snowfall, some notes and an example
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1985
[PDF-1.32 MB]
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Description:"A lake effect snowfall along the Wasatch Front is typically a post cold frontal event in which the duration of snowfall downwind of the lee shore is extended in cold, northwest flow. Where one would normally expect snowfall to end with the passage of the upper level trough, lake effect snows usually continue for several hours after that event"--Introduction.
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Content Notes:David M. Carpenter.
Includes bibliographical references (page 16).
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Rights Information:Public Domain
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Compliance:Library
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