Upslope Flow Dynamics
Upslope Flow Dynamics is a meteorological process in which moist air is forced to ascend along a topographic slope, leading to adiabatic cooling, condensation, and orographic precipitation, and is distinguished from other atmospheric lifting mechanisms by its direct dependence on terrain-induced vertical motion.
73
Publications
4K
Citations
221
Authors
111
Institutions
Publications per year
2017–2026
9
Parents
73
1–5 of 73
221
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Leibniz Institute for Baltic Sea Research Warnemünde, Germany
3 publications · 123 citations
3
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2
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Cooperative Institute for Research in Environmental Sciences, United States
2 publications · 38 citations
2
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1–5 of 221
111

NSF National Center for Atmospheric Research
Boulder, United States
7 h-index
13 publications
602 citations
University of Colorado Boulder
Boulder, United States
5 h-index
13 publications
445 citations
Colorado State University
Fort Collins, United States
5 h-index
14 publications
1.4K citations
Cooperative Institute for Research in Environmental Sciences
Boulder, United States
4 h-index
9 publications
720 citations
National Oceanic and Atmospheric Administration
Washington, United States
4 h-index
11 publications
244 citations

Pacific Northwest National Laboratory
Richland, United States
3 h-index
4 publications
120 citations

Leibniz Institute for Baltic Sea Research Warnemünde
Warnemünde, Germany
3 h-index
6 publications
246 citations

McGill University
Montreal, Canada
3 h-index
7 publications
183 citations
1–8 of 111
15 publications · 1.1K citations
15
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9 publications · 442 citations
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JGR · 7 publications · 446 citations
7
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3 publications · 128 citations
3
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3 publications · 56 citations
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