Mountain Climate Forcing
Mountain Climate Forcing is a geophysical mechanism that denotes the aggregate influence of orographic features on atmospheric processes, whereby topographic elevation, slope, and aspect differentially modify incident solar radiation, temperature gradients, wind patterns, and precipitation distribution relative to surrounding lowlands.
145
Publications
12.4K
Citations
550
Authors
278
Institutions
Publications per year
2017–2026
51
Parents
145
The influence of climate on the tectonic evolution of mountain belts
K. X. Whipple · Nature Geoscience · 2009 · 632 citations
The altitudinal dependence of recent rapid warming over the Tibetan Plateau
Jun Qin, Kun Yang, Shunlin Liang et al. · Climatic Change · 2009 · 405 citations
1–5 of 145
550
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278

Chinese Academy of Sciences
Beijing, China
28 h-index
121 publications
10.1K citations
Institute of Atmospheric Physics
Beijing, China
18 h-index
53 publications
5.2K citations
University of Chinese Academy of Sciences
Beijing, China
12 h-index
32 publications
1.9K citations

Centre National de la Recherche Scientifique
Paris, France
11 h-index
42 publications
2.2K citations
Institute of Tibetan Plateau Research
Beijing, China
8 h-index
30 publications
3K citations

Nanjing University of Information Science and Technology
Nanjing, China
7 h-index
13 publications
852 citations
Center for Excellence in Tibetan Plateau Earth Sciences
Beijing, China
6 h-index
15 publications
1.3K citations
Chinese Academy of Meteorological Sciences
Beijing, China
5 h-index
15 publications
1.1K citations
1–8 of 278
13 publications · 1.4K citations
13
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9 publications · 1.1K citations
9
h-index
8 publications · 628 citations
8
h-index
4 publications · 69 citations
4
h-index
4 publications · 88 citations
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1–5