Complex Terrain Flow
Complex Terrain Flow is a fluid dynamics phenomenon characterized by the three-dimensional distortion and acceleration of wind flow due to the interaction of atmospheric boundary layer winds with irregular topographic features such as mountains, valleys, and escarpments.
477
Publications
22.3K
Citations
1.4K
Authors
478
Institutions
Publications per year
2017–2026
142
Parents
477
1–5 of 477
1.4K
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University of California, Berkeley, United States
9 publications · 961 citations
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478

NSF National Center for Atmospheric Research
Boulder, United States
25 h-index
117 publications
9.3K citations
Technical University of Denmark
Kongens Lyngby, Denmark
16 h-index
65 publications
4.9K citations
Karlsruhe Institute of Technology
Karlsruhe, Germany
14 h-index
49 publications
3K citations

Lawrence Livermore National Laboratory
Livermore, United States
14 h-index
33 publications
1.5K citations
Kyushu University
Fukuoka, Japan
14 h-index
25 publications
750 citations
University of Colorado Boulder
Boulder, United States
14 h-index
76 publications
8.8K citations

National Laboratory of the Rockies
Golden, United States
12 h-index
55 publications
5.8K citations
National Oceanic and Atmospheric Administration
Washington, United States
12 h-index
64 publications
7K citations
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41 publications · 2K citations
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23 publications · 1.3K citations
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28 publications · 1.5K citations
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23 publications · 985 citations
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17 publications · 1.1K citations
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