Mountain-valley Winds
Mountain–Valley Winds is a thermally driven local atmospheric circulation system distinguished by daytime upslope winds along mountain slopes and nighttime downslope winds toward valley floors, generated by differential heating and cooling of mountainous terrain relative to adjacent air.
408
Publications
18.7K
Citations
1.2K
Authors
445
Institutions
Publications per year
2017–2026
101
Variants
Mountain-valley CirculationMountain-valley Wind Systems
Parents
408
1–5 of 408
1.2K
9
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7
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445

Chinese Academy of Sciences
Beijing, China
21 h-index
110 publications
3.6K citations

NSF National Center for Atmospheric Research
Boulder, United States
13 h-index
45 publications
6.9K citations

Southwest Jiaotong University
Chengdu, China
13 h-index
42 publications
2.2K citations

Universität Innsbruck
Innsbruck, Austria
13 h-index
33 publications
1.5K citations

China Meteorological Administration
Beijing, China
11 h-index
23 publications
1.5K citations

Pacific Northwest National Laboratory
Richland, United States
10 h-index
43 publications
5.8K citations
University of Chinese Academy of Sciences
Beijing, China
10 h-index
21 publications
788 citations
Northwest Institute of Eco-Environment and Resources
Lanzhou, China
9 h-index
43 publications
1.5K citations
1–8 of 445
21 publications · 1K citations
19
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25 publications · 1.3K citations
19
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18 publications · 811 citations
16
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16 publications · 746 citations
14
h-index
12 publications · 419 citations
12
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1–5