Valley Circulations
Valley Circulations is a mesoscale atmospheric circulation pattern characterized by thermally driven upslope winds during the day and downslope winds at night, occurring within mountainous terrain due to differential heating and cooling of valley surfaces relative to surrounding elevations.
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Kun Yang, Toshio Koike, Hideyuki Fujii et al. · Journal of the Meteorological Society of Japan Ser II · 2004 · 127 citations · Full text
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Pacific Northwest National Laboratory
Richland, United States
6 h-index
10 publications
913 citations

Universität Innsbruck
Innsbruck, Austria
6 h-index
18 publications
762 citations
ETH Zurich
Zurich, Switzerland
3 h-index
3 publications
196 citations
Chinese Academy of Meteorological Sciences
Beijing, China
3 h-index
4 publications
437 citations
Los Alamos National Laboratory
Los Alamos, United States
3 h-index
5 publications
244 citations
Colorado State University
Fort Collins, United States
3 h-index
6 publications
200 citations

Centre National de la Recherche Scientifique
Paris, France
3 h-index
10 publications
188 citations
Laboratoire des Écoulements Géophysiques et Industriels
Grenoble, France
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5 publications
236 citations
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