Deep Convective Cloud Processes
Deep Convective Cloud Processes is a meteorological phenomenon characterized by intense, vertically developed cloud systems that transport heat, moisture, and momentum from the lower to the upper troposphere through strong updrafts and downdrafts, distinguishing it from shallow and mid-level convection by its significant vertical extent, anvil formation, and role in tropical weather and climate dynamics.
161
Publications
9.3K
Citations
765
Authors
269
Institutions
Publications per year
2017–2026
50
Parents
161
Intensification of Pacific storm track linked to Asian pollution
Renyi Zhang, Guohui Li, Jiwen Fan et al. · Proceedings of the National Academy of Sciences · 2007 · 246 citations · Full text
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NSF National Center for Atmospheric Research, United States
5 publications · 404 citations
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269

NSF National Center for Atmospheric Research
Boulder, United States
13 h-index
43 publications
4.5K citations
Colorado State University
Fort Collins, United States
11 h-index
29 publications
1.5K citations

Langley Research Center
Hampton, United States
11 h-index
31 publications
2.8K citations
Goddard Space Flight Center
Greenbelt, United States
10 h-index
14 publications
1.4K citations
Jet Propulsion Laboratory
Pasadena, United States
10 h-index
22 publications
1.2K citations
National Oceanic and Atmospheric Administration
Washington, United States
10 h-index
17 publications
1.1K citations
University of Washington
Seattle, United States
9 h-index
20 publications
2K citations

Centre National de la Recherche Scientifique
Paris, France
9 h-index
25 publications
1.2K citations
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JGR · 21 publications · 2K citations
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16 publications · 994 citations
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JGR · 14 publications · 446 citations
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14 publications · 472 citations
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14 publications · 583 citations
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