Lee-side Eddies
Lee-side eddies is a mesoscale atmospheric phenomenon characterized by the formation of counter-rotating vortices on the leeward side of mountainous terrain, resulting from flow separation and dynamic instability in the boundary layer under stable stratification and moderate to strong cross-mountain winds.
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2017–2026
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Robert P. Sharp · The Journal of Geology · 1963 · 334 citations
Sorting in grain flows at the lee side of dunes
Maarten G. Kleinhans · Earth-Science Reviews · 2003 · 147 citations · Full text
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University of Hawaii System
Honolulu, United States
4 h-index
11 publications
389 citations

University of Hawaiʻi at Mānoa
Honolulu, United States
3 h-index
9 publications
405 citations
University of California, Los Angeles
Los Angeles, United States
2 h-index
4 publications
265 citations

Langley Research Center
Hampton, United States
2 h-index
3 publications
53 citations

Stennis Space Center
Bay Saint Louis, United States
2 h-index
3 publications
178 citations
Planetary Science Institute
Tucson, United States
2 h-index
4 publications
265 citations

United States Naval Research Laboratory
Washington, United States
2 h-index
4 publications
230 citations

University of Cape Town
Rondebosch, South Africa
2 h-index
7 publications
502 citations
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JGR · 4 publications · 324 citations
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4 publications · 193 citations
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2 publications · 34 citations
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2 publications · 62 citations
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2 publications · 88 citations
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