Convective Squall Lines
Convective Squall Lines is a mesoscale convective system characterized by a quasi-linear arrangement of thunderstorms with a leading convective line and a trailing stratiform precipitation region, distinguished from other mesoscale convective systems by its organized, elongated structure and coherent wind gust front.
278
Publications
23.6K
Citations
592
Authors
201
Institutions
Publications per year
2017–2026
26
Parents
278
Diurnal Variation of Deep Cumulus Convection
William M. Gray, Robert W. Jacobson · Monthly Weather Review · 1977 · 568 citations · Full text
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NSF National Center for Atmospheric Research, United States
12 publications · 835 citations
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9
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NSF National Center for Atmospheric Research, United States
9 publications · 3.9K citations
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201

NSF National Center for Atmospheric Research
Boulder, United States
32 h-index
91 publications
19.2K citations
University of Washington
Seattle, United States
15 h-index
34 publications
2.1K citations
Colorado State University
Fort Collins, United States
15 h-index
30 publications
2K citations
Goddard Space Flight Center
Greenbelt, United States
14 h-index
25 publications
2.1K citations
NOAA National Severe Storms Laboratory
Norman, United States
9 h-index
14 publications
803 citations

Centre National de la Recherche Scientifique
Paris, France
9 h-index
21 publications
1.8K citations

Pennsylvania State University
State College, United States
8 h-index
13 publications
3.2K citations
University of Oklahoma
Norman, United States
8 h-index
10 publications
765 citations
1–8 of 201
86 publications · 9.3K citations
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77 publications · 7.3K citations
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26 publications · 1.3K citations
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BAMS · 13 publications · 1.3K citations
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9 publications · 251 citations
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