Valley Breezes
Valley Breezes is a diurnal mesoscale atmospheric circulation characterized by upslope and up-valley flows during daytime, driven by differential heating between mountain slopes and the adjacent valley atmosphere, in which warmer air ascends the valley to form a low-pressure zone that draws in air from lower elevations.
32
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1.5K
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154
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80
Institutions
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2017–2026
11
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Diurnal Rainfall Variation in Northeast Brazil
Vernon E. Kousky · Monthly Weather Review · 1980 · 287 citations
Exchange Processes in the Atmospheric Boundary Layer Over Mountainous Terrain
Stefano Serafin, Bianca Adler, Joan Cuxart et al. · Atmosphere · 2018 · 255 citations · Full text
Evening Transition Observations in Phoenix, Arizona
Anthony J. Brazel, Harindra J. S. Fernando, J. C. R. Hunt et al. · Journal of Applied Meteorology · 2005 · 68 citations
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Chinese Academy of Sciences
Beijing, China
4 h-index
10 publications
365 citations
University of Utah
Salt Lake City, United States
4 h-index
7 publications
314 citations
Institute of Atmospheric Physics
Beijing, China
3 h-index
7 publications
226 citations

Nanjing University of Information Science and Technology
Nanjing, China
3 h-index
6 publications
217 citations

China Meteorological Administration
Beijing, China
3 h-index
8 publications
269 citations

University of Trento
Trento, Italy
2 h-index
3 publications
301 citations
Tianjin University
Tianjin, China
2 h-index
9 publications
276 citations

Centre National de la Recherche Scientifique
Paris, France
2 h-index
8 publications
314 citations
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JGR · 4 publications · 152 citations
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4 publications · 370 citations
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2 publications · 34 citations
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2 publications · 63 citations
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2 publications · 131 citations
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