Current Recirculation
Current Recirculation is a fluid dynamical phenomenon within ocean circulation where a portion of a main oceanic current loops back upon itself, forming a closed or semi-closed circular flow that retains and redistributes water masses, properties, and momentum within a localized region.
30
Publications
1.9K
Citations
80
Authors
40
Institutions
Publications per year
2017–2026
3
Parents
30
Laura de Steur, E. Hansen, Cecilie Mauritzen et al. · Deep Sea Research Part I Oceanographic Research Papers · 2014 · 108 citations
1–5 of 30
80
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Woods Hole Oceanographic Institution, United States
2 publications · 329 citations
2
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2
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2
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1–5 of 80
40
Woods Hole Oceanographic Institution
Falmouth, United States
6 h-index
8 publications
822 citations

The University of Western Australia
Perth, Australia
3 h-index
8 publications
640 citations
Politecnico di Milano
Milan, Italy
2 h-index
8 publications
180 citations
STMicroelectronics (Italy)
Milan, Italy
2 h-index
2 publications
45 citations

University of Hawaii System
Honolulu, United States
2 h-index
2 publications
79 citations
University of California San Diego
San Diego, United States
2 h-index
5 publications
707 citations

Scripps Institution of Oceanography
La Jolla, United States
2 h-index
5 publications
707 citations

Bangor University
Bangor, United Kingdom
1 h-index
2 publications
86 citations
1–8 of 40
4 publications · 213 citations
4
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3 publications · 119 citations
3
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2 publications · 67 citations
2
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2 publications · 45 citations
2
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2 publications · 94 citations
2
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1–5