Lee Wave Clouds
Lee Wave Clouds is a type of orographic cloud formation that occurs when stable air flows over mountainous terrain, generating standing gravity waves in the lee side of the obstacle, where clouds form at the wave crests due to adiabatic cooling in the rising limb of the wave.
41
Publications
1.6K
Citations
106
Authors
51
Institutions
Publications per year
2017–2026
0
Variants
Orographic Wave Clouds
Parents
41
M. G. Wurtele, Robert Sharman, Ashis Datta · Annual Review of Fluid Mechanics · 1996 · 135 citations
1–5 of 41
106
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NOAA National Environmental Satellite Data and Information Service, United States
3 publications · 110 citations
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NOAA National Environmental Satellite Data and Information Service, United States
2 publications · 72 citations
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NSF National Center for Atmospheric Research
Boulder, United States
5 h-index
9 publications
398 citations

Centre National de la Recherche Scientifique
Paris, France
3 h-index
14 publications
404 citations
University of Washington
Seattle, United States
3 h-index
3 publications
243 citations
National Oceanic and Atmospheric Administration
Washington, United States
3 h-index
4 publications
118 citations

United States Naval Research Laboratory
Washington, United States
2 h-index
3 publications
87 citations
NOAA National Environmental Satellite Data and Information Service
Silver Spring, United States
2 h-index
5 publications
250 citations
California Institute of Technology
Pasadena, United States
2 h-index
5 publications
453 citations
Jet Propulsion Laboratory
Pasadena, United States
2 h-index
3 publications
142 citations
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7 publications · 314 citations
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6 publications · 261 citations
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JGR · 5 publications · 308 citations
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4 publications · 62 citations
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3 publications · 80 citations
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