Stratiform Cloud Condensation
Stratiform Cloud Condensation is a meteorological process in which widespread, horizontally uniform cloud formation occurs through the gradual cooling of moist air masses below their dew point, distinguished from convective condensation by its stable, layered structure and large-scale, synoptic forcing mechanisms.
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2017–2026
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Minghua Zhang, Wuyin Lin, Christopher S. Bretherton et al. · Journal of Geophysical Research Atmospheres · 2003 · 227 citations · Full text
Seoung Soo Lee, Leo J. Donner, Vaughan T. J. Phillips et al. · Journal of Geophysical Research Atmospheres · 2008 · 173 citations · Full text
Measurements of the chemical composition of stratiform clouds
P. H. Daum, Thomas J. Kelly, Stephen E. Schwartz et al. · Atmospheric Environment (1967) · 1984 · 139 citations
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National Oceanic and Atmospheric Administration, United States
2 publications · 187 citations
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University of Washington
Seattle, United States
7 h-index
13 publications
1.5K citations

NSF National Center for Atmospheric Research
Boulder, United States
3 h-index
5 publications
554 citations
Colorado State University
Fort Collins, United States
2 h-index
3 publications
113 citations

Chinese Academy of Sciences
Beijing, China
2 h-index
5 publications
97 citations
Institute of Atmospheric Physics
Beijing, China
2 h-index
5 publications
97 citations

Stockholm University
Stockholm, Sweden
2 h-index
2 publications
49 citations
University at Albany, State University of New York
Albany, United States
1 h-index
2 publications
24 citations

Lawrence Livermore National Laboratory
Livermore, United States
1 h-index
3 publications
42 citations
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4 publications · 253 citations
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JGR · 3 publications · 470 citations
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3 publications · 927 citations
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2 publications · 22 citations
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2 publications · 87 citations
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