Ekman Convergence
Ekman Convergence is a physical oceanographic phenomenon in which horizontal variations in wind-driven Ekman transport result in a net accumulation of surface water, distinguished by downward vertical motion at the base of the Ekman layer due to mass conservation.
37
Publications
3.7K
Citations
152
Authors
116
Institutions
Publications per year
2017–2026
9
37
1–5 of 37
152
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116
Woods Hole Oceanographic Institution
Falmouth, United States
5 h-index
11 publications
841 citations
Fisheries and Oceans Canada
Ottawa, Canada
3 h-index
10 publications
1.5K citations

National Oceanography Centre
Southampton, United Kingdom
2 h-index
5 publications
1.1K citations
University of Washington Applied Physics Laboratory
Seattle, United States
2 h-index
10 publications
706 citations

Centre National de la Recherche Scientifique
Paris, France
2 h-index
2 publications
972 citations
University of Southampton
Southampton, United Kingdom
2 h-index
2 publications
975 citations
National Institute of Water and Atmospheric Research
Auckland, New Zealand
2 h-index
2 publications
81 citations

University of Hawaiʻi at Mānoa
Honolulu, United States
2 h-index
5 publications
1.1K citations
1–8 of 116
9 publications · 426 citations
9
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6 publications · 754 citations
6
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JGR · 3 publications · 243 citations
3
h-index
2 publications · 278 citations
2
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2 publications · 103 citations
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1–5