Mesoscale Vorticity
Mesoscale Vorticity is a meteorological phenomenon denoting the rotation inherent in atmospheric flows at the mesoscale, characterized by horizontal vorticity structures typically ranging from 2 to 2000 kilometers in spatial extent and arising from localized gradients in wind shear, convection, or topographic influences.
210
Publications
10.6K
Citations
503
Authors
226
Institutions
Publications per year
2017–2026
30
210
1–5 of 210
503
8
h-index
NSF National Center for Atmospheric Research, United States
5 publications · 512 citations
5
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4
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3
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3
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1–5 of 503
226

NSF National Center for Atmospheric Research
Boulder, United States
13 h-index
22 publications
1.5K citations
Colorado State University
Fort Collins, United States
9 h-index
16 publications
378 citations

Pennsylvania State University
State College, United States
8 h-index
21 publications
791 citations

Centre National de la Recherche Scientifique
Paris, France
7 h-index
15 publications
282 citations
Institute of Atmospheric Physics
Beijing, China
6 h-index
17 publications
599 citations
Meteorological Research Institute
Tsukuba, Japan
6 h-index
12 publications
300 citations

Naval Postgraduate School
Monterey, United States
6 h-index
6 publications
380 citations

Chinese Academy of Sciences
Beijing, China
6 h-index
19 publications
612 citations
1–8 of 226
37 publications · 1.6K citations
26
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20 publications · 1.2K citations
18
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13 publications · 773 citations
12
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JGR · 13 publications · 647 citations
11
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10 publications · 1.1K citations
10
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1–5