Eastern Boundary Current Variability
Eastern Boundary Current Variability is a geophysical phenomenon characterized by temporal fluctuations in the strength, position, and structure of poleward-flowing, eastern-boundary-intensified ocean currents within subtropical gyres, driven by wind forcing, coastal upwelling dynamics, and remote climate modes.
114
Publications
7.3K
Citations
393
Authors
187
Institutions
Publications per year
2017–2026
26
114
1–5 of 114
393
GEOMAR Helmholtz Centre for Ocean Research Kiel, Germany
5 publications · 263 citations
5
h-index
4
h-index
3
h-index
NOAA Atlantic Oceanographic and Meteorological Laboratories, United States
3 publications · 118 citations
3
h-index
NOAA Atlantic Oceanographic and Meteorological Laboratories, United States
3 publications · 118 citations
3
h-index
1–5 of 393
187

Christian-Albrechts-Universität zu Kiel
Kiel, Germany
8 h-index
14 publications
1.4K citations
Institut de Recherche pour le Développement
Marseille, France
7 h-index
15 publications
661 citations
Oregon State University
Corvallis, United States
6 h-index
10 publications
956 citations
Woods Hole Oceanographic Institution
Falmouth, United States
6 h-index
10 publications
576 citations

Centre National de la Recherche Scientifique
Paris, France
6 h-index
20 publications
667 citations

Scripps Institution of Oceanography
La Jolla, United States
5 h-index
20 publications
767 citations
The University of Tokyo
Tokyo, Japan
5 h-index
9 publications
516 citations

GEOMAR Helmholtz Centre for Ocean Research Kiel
Kiel, Germany
5 h-index
23 publications
801 citations
1–8 of 187
12 publications · 629 citations
12
h-index
9 publications · 453 citations
9
h-index
9 publications · 497 citations
9
h-index
8 publications · 1.2K citations
8
h-index
JGR · 7 publications · 640 citations
7
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1–5