Abstract
The interactions of the winter lake-effected boundary layer with synoptic systems over Lake Michigan were analyzed. Clouds associated with a retreating surface low-pressure system located north of Maine on 5 December 1997 produced widespread light snow in the Great Lakes region. Bands of precipitation associated with the synoptic system periodically moved across Lake Michigan in a Southerly direction. Interaction of the lake-effect boundary layer with the precipitating synoptic clouds aloft produced a deeper and more vigorous boundary layer, with greater concentrations of snow, which led to increased snow accumulations.
Original language | English (US) |
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Pages | 567-577 |
Number of pages | 11 |
State | Published - 2004 |
Event | 16th Symposium on Boundary Layers and Turbulence - Portland, ME, United States Duration: Aug 9 2004 → Aug 13 2004 |
Other
Other | 16th Symposium on Boundary Layers and Turbulence |
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Country/Territory | United States |
City | Portland, ME |
Period | 8/9/04 → 8/13/04 |
ASJC Scopus subject areas
- Engineering(all)