Foehn Winds is a type of warm, dry downslope wind that occurs on the leeward side of mountain ranges, distinguished by adiabatic compression following the release of latent heat during air ascent and condensation on the windward side.
88
Publications
4.2K
Citations
252
Authors
139
Institutions
Publications per year
2017–2026
26
Variants
FoehnFöhnFöhn Winds
Publications
88
Surface melt and ponding on Larsen C Ice Shelf and the impact of föhn winds
Adrian Luckman, Andrew D. Elvidge, Daniela Jansen et al. · Antarctic Science · 2014 · 138 citations · Full text
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Authors
252
- HA
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- GJ
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- AG
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- AD
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- JK
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1–5 of 252
Institutions
139
Universität Innsbruck
Innsbruck, Austria
11 h-index
28 publications
871 citations
University of East Anglia
Norwich, United Kingdom
6 h-index
10 publications
725 citations
The University of Queensland
Brisbane, Australia
6 h-index
13 publications
721 citations
Nanjing University of Information Science and Technology
Nanjing, China
6 h-index
9 publications
1.1K citations
Met Office
Exeter, United Kingdom
5 h-index
20 publications
654 citations
British Antarctic Survey
Cambridge, United Kingdom
5 h-index
14 publications
836 citations
University of Tsukuba
Tsukuba, Japan
5 h-index
15 publications
460 citations
University of Canterbury
Christchurch, New Zealand
5 h-index
12 publications
450 citations
1–8 of 139
Venues
- Quarterly Journal of the Royal Meteorological Society
10 publications · 428 citations
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- Meteorology and Atmospheric Physics
8 publications · 235 citations
8
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- Weather and Forecasting
7 publications · 261 citations
7
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- Journal of Geophysical Research Atmospheres
JGR · 5 publications · 373 citations
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- Monthly Weather Review
4 publications · 121 citations
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