Stratiform Precipitation Processes is a meteorological phenomenon characterized by widespread, horizontally extensive cloud formations that produce gradual and uniform precipitation, primarily through slow, large-scale ascent of air in stable atmospheric conditions, differentiating it from convective processes driven by localized buoyant updrafts.
351
Publications
24.1K
Citations
964
Authors
328
Institutions
Publications per year
2017–2026
87
Parents
Publications
351
1–5 of 351
Authors
964
- RA
24
h-index
- RH
12
h-index
- SA
9
h-index
- YF
8
h-index
- MD
6
h-index
1–5 of 964
Institutions
328
University of Washington
Seattle, United States
26 h-index
51 publications
5.8K citations
Colorado State University
Fort Collins, United States
23 h-index
65 publications
5K citations
NSF National Center for Atmospheric Research
Boulder, United States
18 h-index
39 publications
2.7K citations
Institute of Atmospheric Physics
Beijing, China
14 h-index
28 publications
988 citations
Chinese Academy of Sciences
Beijing, China
14 h-index
29 publications
960 citations
Goddard Space Flight Center
Greenbelt, United States
13 h-index
34 publications
6K citations
NOAA National Severe Storms Laboratory
Norman, United States
12 h-index
23 publications
1.3K citations
University of Oklahoma
Norman, United States
12 h-index
32 publications
1.1K citations
1–8 of 328
Venues
- Journal of the Atmospheric Sciences
57 publications · 5.2K citations
37
h-index
- Monthly Weather Review
49 publications · 4.7K citations
29
h-index
- Quarterly Journal of the Royal Meteorological Society
24 publications · 1.4K citations
19
h-index
- Journal of Geophysical Research Atmospheres
JGR · 24 publications · 1.4K citations
19
h-index
- Journal of Climate
15 publications · 1.1K citations
15
h-index
1–5