Foehn Effects
Foehn Effects is a meteorological phenomenon characterized by the warming and drying of air masses descending on the leeward side of mountain ranges, resulting from adiabatic compression following orographic ascent and precipitation on the windward side.
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2K
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200
Authors
118
Institutions
Publications per year
2017–2026
20
Variants
Foehn EffectFöhn EffectFöhn Effects
Parents
44
The Northwestern Argentinean Low: A Study of Two Typical Events
Marcelo E. Seluchi, Celeste Saulo, Matilde Nicolini et al. · Monthly Weather Review · 2003 · 138 citations · Full text
Irina Gorodetskaya, Claudio Durán-Alarcón, Sergi González et al. · npj Climate and Atmospheric Science · 2023 · 98 citations · Full text
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118

Centre National de la Recherche Scientifique
Paris, France
5 h-index
12 publications
922 citations
Institut des Géosciences de l'Environnement
Saint-Martin-d'Hères, France
4 h-index
7 publications
535 citations
Institute of Atmospheric Physics
Beijing, China
3 h-index
5 publications
329 citations
University of Liège
Liège, Belgium
3 h-index
7 publications
290 citations

Chinese Academy of Sciences
Beijing, China
3 h-index
5 publications
329 citations
University of Wisconsin–Madison
Madison, United States
3 h-index
3 publications
200 citations
ETH Zurich
Zurich, Switzerland
3 h-index
5 publications
311 citations

University of Leeds
Leeds, United Kingdom
3 h-index
4 publications
102 citations
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JGR · 5 publications · 324 citations
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4 publications · 294 citations
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3 publications · 161 citations
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2 publications · 41 citations
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2 publications · 76 citations
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