Rain Shadow Effects
Rain Shadow Effects is a climatological phenomenon in which a mountain range causes a significant reduction in precipitation on its leeward side, resulting in drier conditions relative to the windward side due to orographic lifting and subsequent moisture depletion of air masses.
80
Publications
4K
Citations
272
Authors
121
Institutions
Publications per year
2017–2026
23
Variants
Rain ShadowRain Shadow Effect
Parents
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121
Stanford University
Stanford, United States
6 h-index
10 publications
866 citations
University of California, Davis
Davis, United States
5 h-index
9 publications
348 citations

Indian Institute of Tropical Meteorology
Pune, India
5 h-index
36 publications
596 citations
United States Geological Survey
Reston, United States
4 h-index
6 publications
453 citations
University of Washington
Seattle, United States
4 h-index
9 publications
406 citations

Consejo Nacional de Investigaciones Científicas y Técnicas
Buenos Aires, Argentina
3 h-index
8 publications
442 citations

Chinese Academy of Sciences
Beijing, China
3 h-index
7 publications
190 citations

University of Otago
Dunedin, New Zealand
3 h-index
7 publications
414 citations
1–8 of 121
4 publications · 384 citations
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3 publications · 82 citations
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2 publications · 45 citations
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AJB · 2 publications · 47 citations
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2 publications · 24 citations
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