Surface Aerodynamic Drag
Surface Aerodynamic Drag is a micrometeorological force representing the resistive interaction between a planet's surface and the overlying airflow, distinguished by its dependence on surface roughness, wind speed, and atmospheric stability conditions.
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7.7K
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446
Authors
190
Institutions
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2017–2026
49
Parents
142
Drag and drag partition on rough surfaces
Michael Raupach · Boundary-Layer Meteorology · 1992 · 792 citations
Climate model shows large-scale wind and solar farms in the Sahara increase rain and vegetation
Yan Li, Eugenia Kalnay, Safa Motesharrei et al. · Science · 2018 · 269 citations · Full text
V. K. Makin, Vladimir Kudryavtsev, C. Mastenbroek · Boundary-Layer Meteorology · 1995 · 186 citations
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NSF National Center for Atmospheric Research, United States
2 publications · 59 citations
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190

Chinese Academy of Sciences
Beijing, China
6 h-index
15 publications
559 citations

Northwestern Polytechnical University
Xi'an, China
4 h-index
7 publications
720 citations

Centre National de la Recherche Scientifique
Paris, France
4 h-index
10 publications
430 citations
Institute of Atmospheric Physics
Beijing, China
3 h-index
5 publications
450 citations

Zhejiang University of Technology
Hangzhou, China
3 h-index
8 publications
205 citations

NSF National Center for Atmospheric Research
Boulder, United States
3 h-index
3 publications
77 citations

Harbin Engineering University
Harbin, China
3 h-index
8 publications
456 citations
Institute of Applied Physics
Nizhny Novgorod, Russia
2 h-index
9 publications
837 citations
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JGR · 6 publications · 957 citations
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6 publications · 1.3K citations
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AST · 5 publications · 194 citations
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5 publications · 209 citations
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4 publications · 237 citations
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