Surface Drift
Surface Drift is a geophysical phenomenon denoting the net movement of surface ocean water induced by wind stress and modified by the Coriolis effect, distinguished from deeper current systems by its direct responsiveness to atmospheric forcing and its role in the upper-layer transport of heat, nutrients, and marine debris.
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13.2K
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680
Authors
311
Institutions
Publications per year
2017–2026
45
Variants
Surface Current
Parents
255
Jin Wu · Journal of Fluid Mechanics · 1975 · 369 citations
Klaus Wyrtki, Lorenz Magaard, James G. Hager · Journal of Geophysical Research Atmospheres · 1976 · 303 citations
Ocean convergence and the dispersion of flotsam
Eric A. D’Asaro, Andrey Shcherbina, Jody Klymak et al. · Proceedings of the National Academy of Sciences · 2018 · 301 citations · Full text
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University of Miami
Coral Gables, United States
11 h-index
39 publications
4.6K citations

Centre National de la Recherche Scientifique
Paris, France
9 h-index
27 publications
1.8K citations

Scripps Institution of Oceanography
La Jolla, United States
8 h-index
11 publications
622 citations
Ifremer
Brest, France
8 h-index
22 publications
1.4K citations
Woods Hole Oceanographic Institution
Falmouth, United States
8 h-index
10 publications
984 citations

Norwegian Meteorological Institute
Oslo, Norway
7 h-index
13 publications
867 citations

University of Oslo
Oslo, Norway
7 h-index
12 publications
539 citations

Stennis Space Center
Bay Saint Louis, United States
7 h-index
11 publications
883 citations
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27 publications · 1.4K citations
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JGR · 20 publications · 1.9K citations
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12 publications · 619 citations
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11 publications · 1.3K citations
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6 publications · 205 citations
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