Mountain-Valley Circulations is a mesoscale atmospheric circulation system characterized by thermally driven slope and valley winds that develop due to differential heating and cooling of mountain and valley surfaces, distinguishing it from larger-scale synoptic flows and other terrain-induced wind systems by its diurnal cycle and confinement within mountainous and valley topography.
164
Publications
8.8K
Citations
518
Authors
218
Institutions
Publications per year
2017–2026
27
Publications
164
1–5 of 164
Authors
518
- MW
8
h-index
- AG
6
h-index
- GZ
5
h-index
- YM
4
h-index
- GJ
3
h-index
1–5 of 518
Institutions
218
Universität Innsbruck
Innsbruck, Austria
9 h-index
32 publications
1.5K citations
Chinese Academy of Sciences
Beijing, China
8 h-index
35 publications
1.7K citations
Chinese Academy of Meteorological Sciences
Beijing, China
8 h-index
13 publications
893 citations
Institute of Atmospheric Physics
Beijing, China
6 h-index
10 publications
1K citations
University of Washington
Seattle, United States
6 h-index
10 publications
736 citations
Météo-France
Toulouse, France
5 h-index
13 publications
263 citations
ETH Zurich
Zurich, Switzerland
5 h-index
6 publications
439 citations
Institute of Tibetan Plateau Research
Beijing, China
5 h-index
11 publications
352 citations
1–8 of 218
Venues
- Quarterly Journal of the Royal Meteorological Society
18 publications · 746 citations
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- Meteorology and Atmospheric Physics
10 publications · 740 citations
10
h-index
- Monthly Weather Review
10 publications · 397 citations
10
h-index
- Boundary-Layer Meteorology
7 publications · 303 citations
7
h-index
- Journal of the Atmospheric Sciences
6 publications · 668 citations
6
h-index
1–5