Thermally Driven Circulations
Thermally Driven Circulations is a meteorological phenomenon in which local winds are generated due to differential heating between mountain and valley surfaces, creating a pressure gradient that drives air movement upslope during the day and downslope at night.
107
Publications
6.5K
Citations
248
Authors
140
Institutions
Publications per year
2017–2026
9
Variants
Thermally Driven Wind Systems
Parents
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248
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140
Colorado State University
Fort Collins, United States
6 h-index
16 publications
2.6K citations
University of Utah
Salt Lake City, United States
6 h-index
13 publications
259 citations

NSF National Center for Atmospheric Research
Boulder, United States
5 h-index
10 publications
268 citations
Los Alamos National Laboratory
Los Alamos, United States
4 h-index
5 publications
430 citations

Universität Innsbruck
Innsbruck, Austria
4 h-index
10 publications
672 citations
University of Wisconsin–Madison
Madison, United States
3 h-index
4 publications
48 citations
Arizona State University
Tempe, United States
3 h-index
9 publications
202 citations

Centre National de la Recherche Scientifique
Paris, France
3 h-index
22 publications
610 citations
1–8 of 140
14 publications · 2K citations
13
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11 publications · 756 citations
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JAMC · 9 publications · 252 citations
9
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7 publications · 282 citations
7
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5 publications · 349 citations
5
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1–5