Terrain-Induced Circulation is a meteorological phenomenon characterized by localized atmospheric circulation patterns that arise due to the differential heating and cooling of air in proximity to complex topographic features, such as mountains and valleys, where the interaction between solar insolation, surface temperature gradients, and gravitational forces drives thermally direct winds along sloped terrain.
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69
Authors
45
Institutions
Publications per year
2017–2026
3
Parents
Publications
23
1–5 of 23
Authors
69
- MS
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Institutions
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Colorado State University
Fort Collins, United States
3 h-index
8 publications
1.6K citations
University of Alabama in Huntsville
Huntsville, United States
2 h-index
5 publications
205 citations
National Taiwan University
Taipei, Taiwan
2 h-index
3 publications
183 citations
NSF National Center for Atmospheric Research
Boulder, United States
2 h-index
2 publications
215 citations
University of Nebraska–Lincoln
Lincoln, United States
1 h-index
1 publications
26 citations
Universidade de São Paulo
São Paulo, Brazil
1 h-index
1 publications
88 citations
National Oceanic and Atmospheric Administration
Washington, United States
1 h-index
1 publications
175 citations
Universidade dos Açores
Ponta Delgada, Portugal
1 h-index
2 publications
82 citations
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Venues
- Monthly Weather Review
6 publications · 758 citations
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- Journal of the Atmospheric Sciences
3 publications · 137 citations
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- Journal of Climate
2 publications · 58 citations
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- Bulletin of the American Meteorological Society
BAMS · 2 publications · 219 citations
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- Boundary-Layer Meteorology
2 publications · 86 citations
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