Frontogenetical Circulation
Frontogenetical Circulation is a secondary meridional circulation that arises in the vicinity of a developing front, driven by the asymmetric contraction of isotherms due to horizontal deformation and shear in the ageostrophic wind field, thereby intensifying thermal gradients during frontogenesis.
17
Publications
872
Citations
36
Authors
19
Institutions
Publications per year
2017–2026
0
17
1–5 of 17
36
University at Albany, State University of New York, United States
3 publications · 127 citations
3
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2
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2
h-index
1
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1
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1–5 of 36
19
Massachusetts Institute of Technology
Cambridge, United States
2 h-index
2 publications
183 citations

Saint Louis University
St Louis, United States
2 h-index
6 publications
158 citations
Albany State University
Albany, United States
1 h-index
1 publications
11 citations
NOAA National Environmental Satellite Data and Information Service
Silver Spring, United States
1 h-index
1 publications
11 citations

Cooperative Institute for Mesoscale Meteorological Studies
Norman, United States
1 h-index
1 publications
24 citations
University of Illinois Urbana-Champaign
Urbana, United States
1 h-index
2 publications
38 citations
University at Albany, State University of New York
Albany, United States
1 h-index
1 publications
11 citations
National Taiwan Normal University
Taipei, Taiwan
1 h-index
1 publications
10 citations
1–8 of 19
5 publications · 120 citations
5
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5 publications · 91 citations
5
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5 publications · 333 citations
5
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1 publications · 303 citations
1
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1 publications · 25 citations
1
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1–5