Storm-scale Circulations
Storm-Scale Circulations is a meteorological phenomenon characterized by organized, persistent air movements within a thunderstorm that operate at spatial scales ranging from a few kilometers to several tens of kilometers, driven primarily by buoyancy and vertical wind shear, and responsible for the development and maintenance of supercellular structures and tornadogenesis.
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457
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2017–2026
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David C. Dowell, Louis J. Wicker, Chris Snyder · Monthly Weather Review · 2011 · 220 citations · Full text
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NSF National Center for Atmospheric Research, United States
6 publications · 436 citations
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University of Oklahoma
Norman, United States
20 h-index
42 publications
3.1K citations
NOAA National Severe Storms Laboratory
Norman, United States
18 h-index
47 publications
3K citations
NOAA National Weather Service
Silver Spring, United States
12 h-index
16 publications
1.7K citations

Cooperative Institute for Mesoscale Meteorological Studies
Norman, United States
11 h-index
19 publications
1.3K citations

Pennsylvania State University
State College, United States
9 h-index
24 publications
1.4K citations

NSF National Center for Atmospheric Research
Boulder, United States
8 h-index
14 publications
817 citations

China Meteorological Administration
Beijing, China
7 h-index
17 publications
834 citations
Texas Tech University
Lubbock, United States
7 h-index
13 publications
685 citations
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60 publications · 3.3K citations
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BAMS · 8 publications · 257 citations
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