Pacific Equatorial Current Variability is a geophysical phenomenon characterized by temporal fluctuations in the strength and direction of zonal surface currents along the equatorial Pacific Ocean, driven primarily by variations in wind stress and ocean-atmosphere interactions.
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Source waters of the Pacific Equatorial Undercurrent
Mizuki Tsuchiya, Roger Lukas, Rana A. Fine et al. · Progress In Oceanography · 1989 · 296 citations
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120
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Institute of Oceanology
Qingdao, China
12 h-index
39 publications
1.1K citations
Chinese Academy of Sciences
Beijing, China
10 h-index
30 publications
927 citations
University of Hawaii System
Honolulu, United States
7 h-index
9 publications
1.3K citations
Qingdao National Laboratory for Marine Science and Technology
Qingdao, China
5 h-index
14 publications
422 citations
Scripps Institution of Oceanography
La Jolla, United States
5 h-index
9 publications
644 citations
University of Chinese Academy of Sciences
Beijing, China
5 h-index
8 publications
241 citations
Fujian Institute of Oceanography
Amoy, China
3 h-index
3 publications
62 citations
Laboratoire d'Océanographie et du Climat : Expérimentations et Approches Numériques
Paris, France
2 h-index
3 publications
109 citations
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- Journal of Geophysical Research Atmospheres
JGR · 8 publications · 549 citations
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- Journal of Physical Oceanography
6 publications · 366 citations
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- Journal of Geophysical Research Oceans
6 publications · 161 citations
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- Progress In Oceanography
3 publications · 537 citations
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- Chinese Journal of Oceanology and Limnology
3 publications · 44 citations
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