Slope-driven Wind Systems
Slope-Driven Wind Systems is a meteorological phenomenon characterized by thermally induced airflows that develop along mountain slopes due to differential heating and cooling, distinguishing it from large-scale synoptic winds by its localized topographic dependence and diurnal reversal pattern.
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Publications
300
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26
Authors
14
Institutions
Publications per year
2017–2026
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8
Local wind system in the Rongbuk Valley on the northern slope of Mt. Everest
Han Zou, Libo Zhou, Shupo Ma et al. · Geophysical Research Letters · 2008 · 43 citations
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Universität Innsbruck
Innsbruck, Austria
2 h-index
5 publications
157 citations

University of KwaZulu-Natal
Durban, South Africa
1 h-index
1 publications
40 citations
Earth Science Institute of the Slovak Academy of Sciences
Bratislava, Slovakia
1 h-index
1 publications
23 citations
Deutsches Zentrum für Luft- und Raumfahrt e. V. (DLR)
Cologne, Germany
1 h-index
1 publications
53 citations
Central Institution for Meteorology and Geodynamics
Vienna, Austria
1 h-index
1 publications
53 citations

University of the Witwatersrand
Johannesburg, South Africa
1 h-index
1 publications
40 citations
Institute of Atmospheric Physics
Beijing, China
1 h-index
8 publications
344 citations
University of Utah
Salt Lake City, United States
1 h-index
3 publications
30 citations
1–8 of 14
JAMC · 1 publications · 10 citations
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JGR · 1 publications · 40 citations
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1 publications · 43 citations
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1 publications · 40 citations
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1 publications · 65 citations
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