Mixed Layer Circulation
Mixed Layer Circulation is a wind-driven ocean circulation process that occurs within the upper, homogenized layer of the ocean where turbulent mixing homogenizes temperature and salinity, distinguishing it from deeper, stratified circulations by its direct responsiveness to surface wind stress and buoyancy forcing.
114
Publications
7.4K
Citations
339
Authors
148
Institutions
Publications per year
2017–2026
19
Parents
114
1–5 of 114
339
4
h-index
University of Maryland Center for Environmental Science, United States
3 publications · 303 citations
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2
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2
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University of Maryland Center for Environmental Science, United States
2 publications · 108 citations
2
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1–5 of 339
148
Woods Hole Oceanographic Institution
Falmouth, United States
11 h-index
18 publications
1.8K citations
Institute of Oceanology
Qingdao, China
5 h-index
24 publications
556 citations

British Antarctic Survey
Cambridge, United Kingdom
4 h-index
7 publications
328 citations
National Oceanic and Atmospheric Administration
Washington, United States
4 h-index
10 publications
527 citations
NOAA Atlantic Oceanographic and Meteorological Laboratories
Miami, United States
4 h-index
4 publications
304 citations
South China Sea Institute Of Oceanology
Guangzhou, China
4 h-index
20 publications
468 citations

Lamont-Doherty Earth Observatory
Sparkill, United States
4 h-index
8 publications
850 citations
Natural Environment Research Council
Swindon, United Kingdom
3 h-index
8 publications
526 citations
1–8 of 148
30 publications · 1.7K citations
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JGR · 14 publications · 1.3K citations
13
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6 publications · 159 citations
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3 publications · 336 citations
3
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3 publications · 258 citations
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