Upslope Flows
Upslope Flows is a thermally driven atmospheric boundary-layer wind phenomenon characterized by the ascent of air parallel to terrain slope during daytime heating, distinguishing it from other slope wind regimes by its diurnal timing, directionality, and reliance on surface-induced convective instability.
181
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14.3K
Citations
548
Authors
244
Institutions
Publications per year
2017–2026
31
Variants
Anabatic Flows
181
Orographic effects on precipitating clouds
Robert A. Houze · Reviews of Geophysics · 2011 · 951 citations · Full text
Keith Beven, Jim Freer · Hydrological Processes · 2001 · 376 citations
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Leibniz Institute for Baltic Sea Research Warnemünde, Germany
3 publications · 123 citations
3
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1–5 of 548
244
Colorado State University
Fort Collins, United States
9 h-index
28 publications
2.8K citations
University of Colorado Boulder
Boulder, United States
8 h-index
19 publications
825 citations

NSF National Center for Atmospheric Research
Boulder, United States
8 h-index
15 publications
572 citations

Chinese Academy of Sciences
Beijing, China
6 h-index
14 publications
1.1K citations
Cooperative Institute for Research in Environmental Sciences
Boulder, United States
6 h-index
14 publications
1.1K citations
Goddard Space Flight Center
Greenbelt, United States
5 h-index
6 publications
519 citations

McGill University
Montreal, Canada
5 h-index
10 publications
580 citations
National Oceanic and Atmospheric Administration
Washington, United States
5 h-index
15 publications
320 citations
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22 publications · 1.4K citations
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JGR · 18 publications · 1.6K citations
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15 publications · 962 citations
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8 publications · 373 citations
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8 publications · 375 citations
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