Shallow Convective Rainfall
Shallow Convective Rainfall is a type of precipitation arising from buoyancy-driven, relatively low-altitude cloud convection characterized by limited vertical development and the absence of ice-phase processes, typically occurring in warm rain regimes where droplet growth is dominated by collision and coalescence within clouds that rarely extend above the 0°C isotherm.
39
Publications
2K
Citations
126
Authors
80
Institutions
Publications per year
2017–2026
12
Parents
39
1–5 of 39
126
4
h-index
Cooperative Institute for Research in Environmental Sciences, United States
2 publications · 185 citations
2
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Rutgers, The State University of New Jersey, United States
2 publications · 317 citations
2
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2
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2
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1–5 of 126
80
University of Colorado Boulder
Boulder, United States
4 h-index
7 publications
451 citations
Texas A&M University
College Station, United States
4 h-index
5 publications
332 citations
University of Washington
Seattle, United States
4 h-index
8 publications
549 citations
Goddard Space Flight Center
Greenbelt, United States
3 h-index
5 publications
661 citations

Indian Institute of Science Bangalore
Bengaluru, India
3 h-index
4 publications
173 citations
University of California, Los Angeles
Los Angeles, United States
2 h-index
2 publications
64 citations
Rutgers, The State University of New Jersey
New Brunswick, United States
2 h-index
4 publications
634 citations
Royal Netherlands Meteorological Institute
De Bilt, The Netherlands
2 h-index
2 publications
28 citations
1–8 of 80
JGR · 6 publications · 195 citations
6
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5 publications · 189 citations
5
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4 publications · 212 citations
4
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3 publications · 604 citations
3
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2 publications · 172 citations
2
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1–5