Boundary Current Upwelling
Boundary Current Upwelling is a physical oceanographic process in which wind-driven divergence along eastern boundaries of ocean basins induces the upward movement of cold, nutrient-rich deep water to the surface, distinguishing it from other upwelling types by its geographic confinement to coastal boundary currents and its dynamical linkage to large-scale wind stress curl and Ekman transport.
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2017–2026
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Ryan R. Rykaczewski, John P. Dunne, William J. Sydeman et al. · Geophysical Research Letters · 2015 · 288 citations · Full text
Deep South China Sea circulation
Guihua Wang, Shang‐Ping Xie, Tangdong Qu et al. · Geophysical Research Letters · 2011 · 233 citations · Full text
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Woods Hole Oceanographic Institution
Falmouth, United States
10 h-index
14 publications
609 citations
Universidade Federal Fluminense
Niterói, Brazil
5 h-index
20 publications
616 citations
Massachusetts Institute of Technology
Cambridge, United States
4 h-index
4 publications
374 citations
Institut de Recherche pour le Développement
Marseille, France
3 h-index
4 publications
211 citations
Jet Propulsion Laboratory
Pasadena, United States
3 h-index
5 publications
626 citations

University of Cape Town
Rondebosch, South Africa
3 h-index
6 publications
405 citations

Scripps Institution of Oceanography
La Jolla, United States
2 h-index
3 publications
128 citations

UNSW Sydney
Sydney, Australia
2 h-index
5 publications
525 citations
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JGR · 4 publications · 212 citations
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