Downslope Windstorms
Downslope Windstorms is a type of regional atmospheric phenomenon within mountain wind systems characterized by strong, gusty, and often turbulent winds that descend from mountainous terrain through the acceleration of air masses forced over topographic barriers and amplified by gravity-driven flow and resonance effects in stably stratified layers.
121
Publications
5.6K
Citations
269
Authors
114
Institutions
Publications per year
2017–2026
32
121
Ronald B. Smith · Journal of the Atmospheric Sciences · 1985 · 350 citations · Full text
Terry L. Clark, Richard D. Farley · Journal of the Atmospheric Sciences · 1984 · 349 citations · Full text
Natural Sciences, Meteorology, Computational Fluid Dynamics +10
1–5 of 121
269
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NSF National Center for Atmospheric Research, United States
5 publications · 955 citations
5
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1–5 of 269
114

NSF National Center for Atmospheric Research
Boulder, United States
10 h-index
21 publications
2.6K citations

University of Toronto
Toronto, Canada
8 h-index
13 publications
510 citations
NOAA National Weather Service
Silver Spring, United States
8 h-index
15 publications
388 citations
University of Utah
Salt Lake City, United States
6 h-index
14 publications
705 citations
University of Washington
Seattle, United States
5 h-index
8 publications
304 citations

United States Naval Research Laboratory
Washington, United States
5 h-index
7 publications
322 citations
University of Bergen
Bergen, Norway
5 h-index
5 publications
150 citations
University at Albany, State University of New York
Albany, United States
4 h-index
7 publications
274 citations
1–8 of 114
27 publications · 2.4K citations
19
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15 publications · 632 citations
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14 publications · 564 citations
13
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6 publications · 330 citations
6
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7 publications · 218 citations
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