Katabatic Wind Formation
Katabatic Wind Formation is a meteorological phenomenon characterized by the generation of downslope winds due to the gravitational flow of cold, dense air masses originating from elevated cooling surfaces, distinguishing it from other wind formation mechanisms by its thermally driven, topographically channeled descent.
35
Publications
1.5K
Citations
109
Authors
54
Institutions
Publications per year
2017–2026
2
Parents
35
Downward transport of ozone‐rich air near Mt. Everest
Tong Zhu, Weili Lin, Yu Song et al. · Geophysical Research Letters · 2006 · 70 citations · Full text
1–5 of 35
109
3
h-index
2
h-index
National Centre of Scientific Research "Demokritos", Greece
2 publications · 38 citations
2
h-index
National Centre of Scientific Research "Demokritos", Greece
2 publications · 82 citations
2
h-index
2
h-index
1–5 of 109
54
University of Oklahoma
Norman, United States
4 h-index
10 publications
350 citations
Utrecht University
Utrecht, The Netherlands
3 h-index
6 publications
284 citations
Met Office
Exeter, United Kingdom
2 h-index
3 publications
140 citations

Centre National de la Recherche Scientifique
Paris, France
2 h-index
17 publications
909 citations
National Centre of Scientific Research "Demokritos"
Athens, Greece
2 h-index
3 publications
64 citations

National and Kapodistrian University of Athens
Athens, Greece
2 h-index
7 publications
112 citations

Université Grenoble Alpes
Saint-Martin-d'Hères, France
2 h-index
8 publications
396 citations

University of Alaska Fairbanks
Fairbanks, United States
2 h-index
2 publications
60 citations
1–8 of 54
6 publications · 235 citations
6
h-index
JGR · 3 publications · 296 citations
3
h-index
3 publications · 168 citations
3
h-index
2 publications · 53 citations
2
h-index
2 publications · 35 citations
2
h-index
1–5