Trailing Stratiform Region is a mesoscale precipitation structure characterized by a broad, gently sloping region of stratiform rainfall that develops behind the convective line in a midlatitude mesoscale convective system, typically associated with a rear-inflow jet and a mesoscale downdraft that destabilizes the trailing anvil, thereby distinguishing it from other types of mesoscale convective system morphology such as leading or parallel stratiform configurations.
49
Publications
2.7K
Citations
105
Authors
42
Institutions
Publications per year
2017–2026
3
Parents
Publications
49
1–5 of 49
Authors
105
- RH
10
h-index
- RA
6
h-index
- WA
6
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- SA
5
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- BF
5
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1–5 of 105
Institutions
42
Colorado State University
Fort Collins, United States
13 h-index
28 publications
1.7K citations
University of Washington
Seattle, United States
6 h-index
11 publications
1K citations
NOAA National Severe Storms Laboratory
Norman, United States
4 h-index
8 publications
281 citations
Goddard Space Flight Center
Greenbelt, United States
4 h-index
5 publications
397 citations
National Oceanic and Atmospheric Administration
Washington, United States
3 h-index
3 publications
251 citations
Cooperative Institute for Mesoscale Meteorological Studies
Norman, United States
3 h-index
6 publications
178 citations
University of Oklahoma
Norman, United States
3 h-index
7 publications
171 citations
NSF National Center for Atmospheric Research
Boulder, United States
3 h-index
5 publications
140 citations
1–8 of 42
Venues
- Monthly Weather Review
19 publications · 1.2K citations
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- Journal of the Atmospheric Sciences
16 publications · 995 citations
15
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- Journal of Geophysical Research Atmospheres
JGR · 5 publications · 170 citations
5
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- Weather and Forecasting
2 publications · 64 citations
2
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- Journal of Applied Meteorology
1 publications · 32 citations
1
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1–5