Warm Rain Processes
Warm Rain Processes is a precipitation formation mechanism in cloud physics characterized by the growth of cloud droplets through collision and coalescence in clouds with temperatures entirely above freezing, distinguishing it from ice-mediated precipitation processes.
236
Publications
16.7K
Citations
611
Authors
221
Institutions
Publications per year
2017–2026
63
236
1–5 of 236
611
NSF National Center for Atmospheric Research, United States
19 publications · 1.8K citations
17
h-index
12
h-index
9
h-index
NSF National Center for Atmospheric Research, United States
9 publications · 599 citations
9
h-index
7
h-index
1–5 of 611
221

NSF National Center for Atmospheric Research
Boulder, United States
30 h-index
67 publications
8.3K citations
Colorado State University
Fort Collins, United States
13 h-index
30 publications
1.8K citations
University of Oklahoma
Norman, United States
13 h-index
35 publications
1.7K citations
Nanjing University
Nanjing, China
12 h-index
40 publications
1.6K citations
The University of Tokyo
Tokyo, Japan
11 h-index
17 publications
1.2K citations
Chinese Academy of Meteorological Sciences
Beijing, China
11 h-index
27 publications
906 citations
University of Illinois Urbana-Champaign
Urbana, United States
10 h-index
23 publications
973 citations
Hebrew University of Jerusalem
Jerusalem, Israel
10 h-index
15 publications
1.8K citations
1–8 of 221
43 publications · 4.4K citations
30
h-index
20 publications · 901 citations
18
h-index
JGR · 20 publications · 810 citations
18
h-index
19 publications · 906 citations
15
h-index
15 publications · 1.9K citations
14
h-index
1–5