Boundary Current Separation
Boundary Current Separation is a geophysical fluid dynamics phenomenon in which a western boundary current detaches from the continental margin due to a local imbalance between pressure gradient and Coriolis forces, marking the transition from a boundary-trapped flow to an offshore, freely propagating jet in large-scale ocean circulation.
47
Publications
2.2K
Citations
95
Authors
60
Institutions
Publications per year
2017–2026
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Florida State University
Tallahassee, United States
6 h-index
11 publications
394 citations
Woods Hole Oceanographic Institution
Falmouth, United States
4 h-index
5 publications
278 citations
Massachusetts Institute of Technology
Cambridge, United States
4 h-index
5 publications
161 citations

UNSW Sydney
Sydney, Australia
3 h-index
9 publications
240 citations
NOAA Geophysical Fluid Dynamics Laboratory
Princeton, United States
3 h-index
3 publications
96 citations

Australian National University
Canberra, Australia
3 h-index
10 publications
246 citations
Institut de Recherche pour le Développement
Marseille, France
2 h-index
4 publications
54 citations

Imperial College London
London, United Kingdom
2 h-index
3 publications
54 citations
1–8 of 60
24 publications · 1.1K citations
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4 publications · 121 citations
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2 publications · 105 citations
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2 publications · 89 citations
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2 publications · 82 citations
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