Synoptic-scale Forcing
Synoptic-Scale Forcing is a meteorological phenomenon representing large-scale atmospheric disturbances, typically associated with mid-latitude weather systems, that initiate or modulate lower-level processes such as convection, precipitation, and boundary layer dynamics through horizontal divergence, vorticity advection, and temperature advection at spatial scales of 1,000 to 3,000 kilometers.
420
Publications
25.9K
Citations
1.2K
Authors
409
Institutions
Publications per year
2017–2026
82
Parents
420
Atmospheric science: an introductory survey
Choice Reviews Online · 2007 · 1.9K citations
Atmospheric Science: An Introductory Survey
R Carey · Physics Bulletin · 1978 · 540 citations
1–5 of 420
1.2K
University at Albany, State University of New York, United States
8 publications · 588 citations
8
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7
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7
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7
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5
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1–5 of 1.2K
409

NSF National Center for Atmospheric Research
Boulder, United States
21 h-index
50 publications
3.9K citations

Chinese Academy of Sciences
Beijing, China
14 h-index
40 publications
2.2K citations
Karlsruhe Institute of Technology
Karlsruhe, Germany
12 h-index
38 publications
1.8K citations
University at Albany, State University of New York
Albany, United States
12 h-index
24 publications
1.9K citations
University of Washington
Seattle, United States
12 h-index
24 publications
1.7K citations
Institute of Atmospheric Physics
Beijing, China
11 h-index
28 publications
976 citations
University of Colorado Boulder
Boulder, United States
11 h-index
22 publications
1.2K citations
Cooperative Institute for Research in Environmental Sciences
Boulder, United States
11 h-index
22 publications
1.6K citations
1–8 of 409
94 publications · 5.9K citations
43
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38 publications · 3.3K citations
30
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30 publications · 2.2K citations
22
h-index
18 publications · 975 citations
15
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14 publications · 596 citations
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1–5