Researchers, including the University of Utah's Jim
Steenburgh and University of Wyoming's Bart Geerts, now report that these
intense snowstorms are fueled by air circulation driven by the heat released by
the lake, and that the shoreline geography of Lake Ontario affects the
formation and location of this circulation. The result? Very heavy snowfall.
The findings, published in three papers, show how the
shorelines of lakes may help forecasters determine the impacts of lake-effect
storms.
"Lake Ontario's east-west orientation allows intense
bands of snow to form," said Ed Bensman, a program director in the
National Science Foundation's (NSF) Division of Atmospheric and Geospace
Sciences, which funded the research. "This study found that the shape of
the lake's shoreline can have an important influence on the low-level winds
that lead to bands of snow for long periods of time -- and to heavy snow
totals. The research team analyzed the strength of these snow bands, and their
formation and persistence. Snow bands were often active for several days."
Source & Link to report:
https://www.sciencedaily.com/releases/2017/11/171115175313.htm
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