Gap Winds
Gap Winds is a localized, channelized low-level wind phenomenon that occurs when synoptic- or mesoscale pressure gradients force air through mountain gaps or constrictions, distinguished from other mountain wind systems by its topographically confined, accelerated flow dynamics.
52
Publications
2.8K
Citations
149
Authors
74
Institutions
Publications per year
2017–2026
11
Variants
Gap Wind
52
1–5 of 52
149
3
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NOAA Pacific Marine Environmental Laboratory, United States
3 publications · 263 citations
3
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3
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2
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2
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1–5 of 149
74
University of Washington
Seattle, United States
8 h-index
13 publications
624 citations
NOAA Pacific Marine Environmental Laboratory
Seattle, United States
6 h-index
10 publications
737 citations

Western University
London, Canada
3 h-index
3 publications
103 citations

Centro de Investigación Científica y de Educación Superior de Ensenada
Ensenada, Mexico
3 h-index
6 publications
74 citations

University of Hawaiʻi at Mānoa
Honolulu, United States
2 h-index
3 publications
374 citations
ETH Zurich
Zurich, Switzerland
2 h-index
2 publications
282 citations

University of British Columbia
Vancouver, Canada
2 h-index
6 publications
145 citations
Universidad Autónoma de Baja California
Mexicali, Mexico
2 h-index
3 publications
41 citations
1–8 of 74
11 publications · 629 citations
11
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5 publications · 163 citations
5
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3 publications · 264 citations
3
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3 publications · 201 citations
3
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JGR · 2 publications · 86 citations
2
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1–5