Orographic Rainfall
Orographic Rainfall is a type of precipitation that results from the adiabatic cooling and condensation of moist air masses as they are forced to ascend over elevated terrain, distinguishing it from other rainfall mechanisms by its direct dependence on topographic uplift.
310
Publications
21.5K
Citations
770
Authors
375
Institutions
Publications per year
2017–2026
53
Parents
310
D. S. Pai, M. Rajeevan, O. P. Sreejith et al. · MAUSAM · 2014 · 2K citations · Full text
Gerard H. Roe · Annual Review of Earth and Planetary Sciences · 2005 · 808 citations
The size distribution of raindrops
A. Best · Quarterly Journal of the Royal Meteorological Society · 1950 · 642 citations
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NSF National Center for Atmospheric Research, United States
6 publications · 752 citations
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6
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375
University of Washington
Seattle, United States
12 h-index
20 publications
3K citations

NSF National Center for Atmospheric Research
Boulder, United States
12 h-index
19 publications
1.2K citations
Met Office
Exeter, United Kingdom
12 h-index
27 publications
2.7K citations
Yale University
New Haven, United States
9 h-index
17 publications
1.8K citations

Centre National de la Recherche Scientifique
Paris, France
9 h-index
25 publications
1.3K citations

Kyoto University
Kyoto, Japan
8 h-index
17 publications
1K citations
Institute of Atmospheric Sciences and Climate
Bologna, Italy
7 h-index
10 publications
423 citations
University of Reading
Reading, United Kingdom
6 h-index
7 publications
344 citations
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35 publications · 3K citations
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28 publications · 1.6K citations
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18 publications · 1.7K citations
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16 publications · 530 citations
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14 publications · 823 citations
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