Anabatic Winds
Anabatic Wind is a thermally driven upslope breeze that occurs when solar heating warms mountain slopes, causing the adjacent air to rise due to density differences, distinguishing it from katabatic and other wind types by its daytime occurrence and upward trajectory along terrain.
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66
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37
Institutions
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2017–2026
2
Variants
Anabatic Wind
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Anabatic Transition ProcessesAnabatic Wind DynamicsAnabatic Wind ForecastingBoundary Layer Structure Over SlopesCloud Formation Associated With Upslope WindsDiurnal Mountain Wind CyclesExtreme Slope Wind EventsField Measurements Of Anabatic WindsHigh-resolution Numerical Modeling Of Upslope WindsKatabatic Transition Processes
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The vertical profile of winds on Titan
M. K. Bird, Michael Allison, S. W. Asmar et al. · Nature · 2005 · 234 citations
Optimal windy sites in Algeria: Potential and perspectives
Hafida Daaou Nedjari, Sabiha Kheder Haddouche, A. Balehouane et al. · Energy · 2017 · 67 citations
Observational consequences of Martian wind regimes
Carl Sagan, Joseph Veverka, P. J. Gierasch · Icarus · 1971 · 54 citations
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37

University of Amsterdam
Amsterdam, The Netherlands
2 h-index
2 publications
40 citations
Radar (United States)
Bothell, United States
1 h-index
1 publications
234 citations
Technische Universität Dresden
Dresden, Germany
1 h-index
1 publications
234 citations
Ruhr University Bochum
Bochum, Germany
1 h-index
1 publications
234 citations

Goddard Institute for Space Studies
New York, United States
1 h-index
1 publications
234 citations
Jet Propulsion Laboratory
Pasadena, United States
1 h-index
1 publications
234 citations
Stanford University
Stanford, United States
1 h-index
1 publications
234 citations
Joint Institute for VLBI ERIC
Dwingeloo, The Netherlands
1 h-index
1 publications
234 citations
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3 publications · 88 citations
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2 publications · 62 citations
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1 publications · 234 citations
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1 publications · 95 citations
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1 publications · 78 citations
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