Complex Terrain Wind Flow
Complex Terrain Wind Flow is a meteorological phenomenon characterized by the distortion and redirection of airflow due to orographic influences in regions of varying elevation, such as mountains and valleys, where terrain-induced turbulence, channeling, and slope effects distinguish it from uniform or flat-terrain wind flow.
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THE TERRAIN-INDUCED ROTOR EXPERIMENT
James D. Doyle, Joachim P. Kuettner, Stephen Mobbs et al. · Bulletin of the American Meteorological Society · 2008 · 212 citations · Full text
The Bolund Experiment, Part I: Flow Over a Steep, Three-Dimensional Hill
Jacob Berg, Jakob Mann, Andreas Bechmann et al. · Boundary-Layer Meteorology · 2011 · 185 citations · Full text
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NSF National Center for Atmospheric Research
Boulder, United States
20 h-index
84 publications
8.1K citations
Technical University of Denmark
Kongens Lyngby, Denmark
19 h-index
79 publications
6K citations

Centre National de la Recherche Scientifique
Paris, France
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41 publications
1.9K citations

Lawrence Livermore National Laboratory
Livermore, United States
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27 publications
1.6K citations
ETH Zurich
Zurich, Switzerland
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49 publications
2.2K citations

National Laboratory of the Rockies
Golden, United States
12 h-index
55 publications
5.9K citations
Kyushu University
Fukuoka, Japan
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17 publications
390 citations
University of Colorado Boulder
Boulder, United States
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83 publications
9K citations
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