Cold-cloud Processes
Cold-Cloud Processes is a precipitation formation mechanism characterized by microphysical interactions, such as deposition, riming, and aggregation, that occur within clouds at temperatures below 0°C, distinguishing it from warm-rain processes that dominate in above-freezing environments.
103
Publications
4.8K
Citations
347
Authors
173
Institutions
Publications per year
2017–2026
22
Parents
103
Influences of cloud photochemical processes on tropospheric ozone
Jos Lelieveld, Paul J. Crutzen · Nature · 1990 · 455 citations
1–5 of 103
347
5
h-index
5
h-index
5
h-index
5
h-index
5
h-index
1–5 of 347
173

NSF National Center for Atmospheric Research
Boulder, United States
8 h-index
23 publications
1.4K citations

Centre National de la Recherche Scientifique
Paris, France
7 h-index
21 publications
1.1K citations
University of Colorado Boulder
Boulder, United States
5 h-index
8 publications
297 citations
University of Washington
Seattle, United States
5 h-index
9 publications
571 citations
Shanghai Institute of Optics and Fine Mechanics
Shanghai, China
4 h-index
37 publications
1.6K citations

Université Laval
Québec, Canada
3 h-index
6 publications
139 citations
Texas A&M University
College Station, United States
3 h-index
4 publications
111 citations

Chinese Academy of Sciences
Beijing, China
3 h-index
5 publications
184 citations
1–8 of 173
10 publications · 866 citations
10
h-index
6 publications · 179 citations
6
h-index
JGR · 6 publications · 235 citations
6
h-index
6 publications · 366 citations
6
h-index
6 publications · 171 citations
6
h-index
1–5