Cold-air Damming
Cold-Air Damming is a mesoscale meteorological phenomenon characterized by the persistence of a shallow, stable layer of cold air trapped against elevated terrain, typically east of mountain barriers, as a result of synoptic-scale anticyclonic flow that inhibits mixing and displacement, thereby distinguishing it from transient cold-air advection or frontal passage.
31
Publications
1.4K
Citations
68
Authors
28
Institutions
Publications per year
2017–2026
0
Variants
Cold Air Damming
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1–5 of 31
68
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University at Albany, State University of New York, United States
3 publications · 263 citations
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3
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2
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2
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1–5 of 68
28

Pennsylvania State University
State College, United States
7 h-index
13 publications
464 citations
North Carolina State University
Raleigh, United States
5 h-index
7 publications
142 citations
University at Albany, State University of New York
Albany, United States
3 h-index
6 publications
526 citations
National Oceanic and Atmospheric Administration
Washington, United States
2 h-index
2 publications
53 citations
NOAA National Weather Service
Silver Spring, United States
2 h-index
4 publications
97 citations
Japan Agency for Marine-Earth Science and Technology
Yokosuka, Japan
1 h-index
2 publications
30 citations
Massachusetts Institute of Technology
Cambridge, United States
1 h-index
2 publications
44 citations
Illinois Archaeological Survey
Champaign, United States
1 h-index
1 publications
95 citations
1–8 of 28
12 publications · 578 citations
11
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10 publications · 440 citations
10
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3 publications · 78 citations
3
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BAMS · 1 publications · 108 citations
1
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1 publications · 31 citations
1
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