Flow Over Mountains is a meteorological phenomenon characterized by the movement and deformation of atmospheric airflow as it encounters and passes over elevated terrain, distinguished from other wind systems by the generation of gravity waves, lee waves, and downslope winds due to orographic forcing.
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2017–2026
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NSF National Center for Atmospheric Research
Boulder, United States
18 h-index
28 publications
1.8K citations
University of Washington
Seattle, United States
14 h-index
32 publications
1.5K citations
Met Office
Exeter, United Kingdom
13 h-index
22 publications
827 citations
Yale University
New Haven, United States
10 h-index
11 publications
1.1K citations
North Carolina State University
Raleigh, United States
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12 publications
543 citations
Météo-France
Toulouse, France
6 h-index
8 publications
339 citations
University of Lisbon
Lisbon, Portugal
6 h-index
12 publications
393 citations
Cooperative Institute for Research in Environmental Sciences
Boulder, United States
5 h-index
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386 citations
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- Journal of the Atmospheric Sciences
57 publications · 2.8K citations
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- Quarterly Journal of the Royal Meteorological Society
42 publications · 2.4K citations
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- Monthly Weather Review
27 publications · 1.4K citations
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- Tellus A Dynamic Meteorology and Oceanography
12 publications · 795 citations
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- Boundary-Layer Meteorology
6 publications · 286 citations
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