Frontal Rainbands is a mesoscale meteorological phenomenon characterized by organized, quasi-linear precipitation bands that develop parallel or near-parallel to mid-latitude frontal boundaries due to sustained lift, frontogenetical forcing, and conditional or conditional symmetric instability within the frontal zone.
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5K
Citations
205
Authors
82
Institutions
Publications per year
2017–2026
3
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1–5 of 99
Authors
205
- PV
18
h-index
- DBDavid B. Parsons
NSF National Center for Atmospheric Research, United States
8 publications · 464 citations
8
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- KA
7
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- JD
6
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- RA
6
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1–5 of 205
Institutions
82
University of Washington
Seattle, United States
16 h-index
50 publications
3.6K citations
University of Reading
Reading, United Kingdom
12 h-index
22 publications
1.4K citations
Met Office
Exeter, United Kingdom
11 h-index
16 publications
1.4K citations
Meteorological Research Institute
Tsukuba, Japan
7 h-index
11 publications
337 citations
NSF National Center for Atmospheric Research
Boulder, United States
5 h-index
7 publications
454 citations
Centre National de la Recherche Scientifique
Paris, France
4 h-index
12 publications
400 citations
Goddard Space Flight Center
Greenbelt, United States
3 h-index
6 publications
183 citations
NOAA National Severe Storms Laboratory
Norman, United States
3 h-index
5 publications
224 citations
1–8 of 82
Venues
- Journal of the Atmospheric Sciences
29 publications · 1.7K citations
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- Quarterly Journal of the Royal Meteorological Society
22 publications · 1.5K citations
17
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- Monthly Weather Review
13 publications · 523 citations
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- Journal of the Meteorological Society of Japan Ser II
10 publications · 328 citations
10
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- Journal of Geophysical Research Atmospheres
JGR · 6 publications · 221 citations
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