Upper Ocean Currents
Upper Ocean Currents is a physical oceanographic phenomenon characterized by the horizontal movement of seawater within the upper layer of the ocean, typically extending from the surface down to depths of approximately 100 to 200 meters, driven primarily by wind stress, buoyancy forces, and the Coriolis effect, and distinguished from deeper ocean currents by its strong interaction with atmospheric forcing and its central role in the transfer of heat, momentum, and mass within the ocean–atmosphere system.
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Publications per year
2017–2026
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Patterns and ecological drivers of ocean viral communities
Jennifer R. Brum, J. Cesar Ignacio‐Espinoza, Simon Roux et al. · Science · 2015 · 827 citations · Full text
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University of California, Los Angeles, United States
6 publications · 625 citations
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341
Woods Hole Oceanographic Institution
Falmouth, United States
20 h-index
43 publications
3.7K citations

Centre National de la Recherche Scientifique
Paris, France
18 h-index
50 publications
14K citations

Scripps Institution of Oceanography
La Jolla, United States
17 h-index
45 publications
3.3K citations
Ifremer
Brest, France
15 h-index
28 publications
2.2K citations

Chinese Academy of Sciences
Beijing, China
14 h-index
52 publications
2.7K citations
Institute of Oceanology
Qingdao, China
14 h-index
65 publications
3.2K citations

University of Hawaiʻi at Mānoa
Honolulu, United States
13 h-index
24 publications
2.6K citations

Université de Bretagne Occidentale
Brest, France
12 h-index
18 publications
2.3K citations
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55 publications · 4.5K citations
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JGR · 50 publications · 3K citations
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24 publications · 1.7K citations
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19 publications · 689 citations
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17 publications · 1.8K citations
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