Upper Ocean Stratification
Upper Ocean Stratification is a geophysical construct that denotes the vertical layering of seawater density in the upper ocean, distinguished by gradients in temperature and salinity that inhibit turbulent mixing and regulate the exchange of heat, momentum, and nutrients between the surface and deeper layers.
389
Publications
26.7K
Citations
1.4K
Authors
462
Institutions
Publications per year
2017–2026
118
389
1–5 of 389
1.4K
7
h-index
6
h-index
National Oceanography Centre, United Kingdom
6 publications · 759 citations
6
h-index
6
h-index
6
h-index
1–5 of 1.4K
462
Woods Hole Oceanographic Institution
Falmouth, United States
24 h-index
46 publications
4.1K citations

Centre National de la Recherche Scientifique
Paris, France
20 h-index
60 publications
6K citations

Scripps Institution of Oceanography
La Jolla, United States
20 h-index
52 publications
3.8K citations
Institut de Recherche pour le Développement
Marseille, France
18 h-index
54 publications
4.7K citations
University of Washington
Seattle, United States
17 h-index
27 publications
2.9K citations
University of Washington Applied Physics Laboratory
Seattle, United States
16 h-index
43 publications
3.1K citations

National Oceanography Centre
Southampton, United Kingdom
15 h-index
28 publications
3.2K citations
University of California San Diego
San Diego, United States
15 h-index
48 publications
3.1K citations
1–8 of 462
52 publications · 5.1K citations
35
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JGR · 39 publications · 3K citations
29
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41 publications · 3.4K citations
27
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35 publications · 1.4K citations
21
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14 publications · 1K citations
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