Boundary Current Mixing is a physical oceanographic process, belonging to the class of lateral mixing phenomena, wherein the transport and blending of water masses are enhanced along density gradients and topographic boundaries due to shear instabilities, turbulence, and eddy activity specific to western or eastern boundary currents.
33
Publications
1.5K
Citations
94
Authors
57
Institutions
Publications per year
2017–2026
7
Parents
Publications
33
1–5 of 33
Authors
94
- IN
3
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3
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- EP
2
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2
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1–5 of 94
Institutions
57
Woods Hole Oceanographic Institution
Falmouth, United States
9 h-index
14 publications
660 citations
University of Southampton
Southampton, United Kingdom
3 h-index
11 publications
740 citations
British Antarctic Survey
Cambridge, United Kingdom
3 h-index
6 publications
537 citations
Centre National de la Recherche Scientifique
Paris, France
3 h-index
5 publications
307 citations
Columbia University
New York, United States
3 h-index
6 publications
194 citations
National Oceanography Centre
Southampton, United Kingdom
3 h-index
14 publications
1K citations
Institut de Recherche pour le Développement
Marseille, France
2 h-index
4 publications
252 citations
Scripps Institution of Oceanography
La Jolla, United States
2 h-index
4 publications
78 citations
1–8 of 57
Venues
- Journal of Physical Oceanography
10 publications · 368 citations
10
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- Journal of Geophysical Research Atmospheres
JGR · 5 publications · 145 citations
5
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- Deep Sea Research Part I Oceanographic Research Papers
4 publications · 164 citations
4
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- Journal of Marine Research
3 publications · 90 citations
3
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- Journal of Sedimentary Research
JSR · 2 publications · 168 citations
2
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1–5