Frontal Circulations
Frontal Circulations is a dynamical oceanic process characterized by coupled cross-frontal exchange flows and secondary circulation cells that emerge at density gradients along oceanic fronts, driven by geostrophic and thermal wind imbalances, and distinct from larger-scale basin circulations or local turbulent mixing.
102
Publications
4.9K
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269
Authors
140
Institutions
Publications per year
2017–2026
14
Variants
Frontal Secondary Circulations
102
Sink or swim, accumulation of biomass at fronts
P. J. S. Franks · Marine Ecology Progress Series · 1992 · 486 citations · Full text
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University at Albany, State University of New York, United States
5 publications · 461 citations
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University of California, Los Angeles, United States
5 publications · 165 citations
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Centro de Investigación Científica y de Educación Superior de Ensenada, Mexico
3 publications · 101 citations
3
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140

NSF National Center for Atmospheric Research
Boulder, United States
7 h-index
9 publications
603 citations
University of Washington
Seattle, United States
4 h-index
7 publications
259 citations
University of California San Diego
San Diego, United States
4 h-index
8 publications
235 citations

Scripps Institution of Oceanography
La Jolla, United States
4 h-index
8 publications
235 citations

Chinese Academy of Sciences
Beijing, China
3 h-index
6 publications
94 citations
Mediterranean Institute for Advanced Studies
Esporles, Spain
3 h-index
6 publications
125 citations
University at Albany, State University of New York
Albany, United States
3 h-index
3 publications
93 citations
Goddard Space Flight Center
Greenbelt, United States
3 h-index
4 publications
588 citations
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13 publications · 463 citations
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11 publications · 629 citations
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10 publications · 443 citations
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9 publications · 638 citations
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JGR · 9 publications · 387 citations
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