Mountain-plain Circulations
Mountain-Plain Circulations is a mesoscale atmospheric circulation system characterized by diurnally reversing wind patterns between mountainous regions and adjacent plains, driven primarily by differential heating and cooling contrasts between elevated terrain and surrounding flatlands.
58
Publications
2.9K
Citations
178
Authors
99
Institutions
Publications per year
2017–2026
11
Variants
Mountain-plain Winds
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99
Colorado State University
Fort Collins, United States
4 h-index
7 publications
270 citations
Institute of Atmospheric Physics
Beijing, China
4 h-index
9 publications
427 citations
University of Utah
Salt Lake City, United States
4 h-index
6 publications
163 citations

Chinese Academy of Sciences
Beijing, China
3 h-index
11 publications
707 citations

Centre National de la Recherche Scientifique
Paris, France
3 h-index
22 publications
798 citations
Universitat de les Illes Balears
Palma, Spain
3 h-index
7 publications
154 citations
Chinese Academy of Meteorological Sciences
Beijing, China
3 h-index
5 publications
202 citations

China Meteorological Administration
Beijing, China
3 h-index
9 publications
117 citations
1–8 of 99
10 publications · 308 citations
10
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3 publications · 86 citations
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3 publications · 181 citations
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3 publications · 157 citations
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1 publications · 16 citations
2
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1–5