Wind-driven Downwelling
Wind-Driven Downwelling is a physical oceanographic process in the genus of wind-driven circulation phenomena, differentiated by the convergence of surface waters due to wind stress curl, resulting in the downward vertical transport of seawater in the upper ocean.
31
Publications
1.8K
Citations
92
Authors
56
Institutions
Publications per year
2017–2026
9
Parents
31
1–5 of 31
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56
Woods Hole Oceanographic Institution
Falmouth, United States
6 h-index
7 publications
383 citations
NOAA Oceanic and Atmospheric Research
Silver Spring, United States
2 h-index
2 publications
180 citations
Oregon State University
Corvallis, United States
2 h-index
4 publications
508 citations

Chinese Academy of Sciences
Beijing, China
2 h-index
7 publications
261 citations
Ocean Institute
Dana Point, United States
2 h-index
2 publications
273 citations
Institute of Oceanology. PP Shirshov Russian Academy of Sciences
Moscow, Russia
2 h-index
6 publications
84 citations
NOAA Pacific Marine Environmental Laboratory
Seattle, United States
1 h-index
1 publications
17 citations

Chinese Academy of Social Sciences
Beijing, China
1 h-index
1 publications
24 citations
1–8 of 56
9 publications · 737 citations
9
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JGR · 2 publications · 126 citations
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2 publications · 119 citations
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2 publications · 29 citations
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1 publications · 15 citations
1
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1–5