Mountain Circulations is a meteorological phenomenon characterized by thermally and topographically driven air movements near mountainous terrain that distinguish it from larger-scale atmospheric circulations through localized vertical and horizontal flow patterns induced by diurnal heating, terrain slope, and valley-channeling effects.
170
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12.6K
Citations
494
Authors
221
Institutions
Publications per year
2017–2026
25
Parents
Publications
170
1–5 of 170
Authors
494
- YM
4
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4
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- RA
4
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4
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3
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1–5 of 494
Institutions
221
Chinese Academy of Sciences
Beijing, China
16 h-index
96 publications
46.7K citations
Institute of Atmospheric Physics
Beijing, China
10 h-index
21 publications
2K citations
University of Chinese Academy of Sciences
Beijing, China
9 h-index
25 publications
621 citations
Center for Excellence in Tibetan Plateau Earth Sciences
Beijing, China
9 h-index
16 publications
1.5K citations
Institute of Tibetan Plateau Research
Beijing, China
9 h-index
39 publications
42.3K citations
Chinese Academy of Meteorological Sciences
Beijing, China
9 h-index
15 publications
861 citations
Colorado State University
Fort Collins, United States
7 h-index
10 publications
465 citations
NSF National Center for Atmospheric Research
Boulder, United States
6 h-index
10 publications
915 citations
1–8 of 221
Venues
- Journal of the Atmospheric Sciences
15 publications · 1.5K citations
15
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- Monthly Weather Review
20 publications · 836 citations
15
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- Journal of the Meteorological Society of Japan Ser II
11 publications · 546 citations
11
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- Quarterly Journal of the Royal Meteorological Society
8 publications · 270 citations
8
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- Bulletin of the American Meteorological Society
BAMS · 5 publications · 354 citations
5
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1–5