Ocean Surface Cooling
Ocean Surface Cooling is a physical oceanographic phenomenon characterized by the reduction in temperature of the upper ocean layer due to heat loss to the atmosphere, primarily driven by turbulent fluxes, radiative processes, and entrainment at the sea surface.
294
Publications
25.9K
Citations
1K
Authors
406
Institutions
Publications per year
2017–2026
83
Parents
294
Recent global-warming hiatus tied to equatorial Pacific surface cooling
Yu Kosaka, Shang‐Ping Xie · Nature · 2013 · 1.7K citations · Full text
James E. Hansen, Makiko Sato, Paul J. Hearty et al. · Atmospheric chemistry and physics · 2016 · 590 citations · Full text
1–5 of 294
1K
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Laboratoire d'Océanographie et du Climat : Expérimentations et Approches Numériques, France
5 publications · 615 citations
5
h-index
NOAA Pacific Marine Environmental Laboratory, United States
5 publications · 671 citations
5
h-index
4
h-index
1–5 of 1K
406

Centre National de la Recherche Scientifique
Paris, France
19 h-index
83 publications
8K citations
Woods Hole Oceanographic Institution
Falmouth, United States
16 h-index
24 publications
3.6K citations
Columbia University
New York, United States
14 h-index
26 publications
3.7K citations
Institut de Recherche pour le Développement
Marseille, France
13 h-index
44 publications
3.6K citations

Chinese Academy of Sciences
Beijing, China
13 h-index
28 publications
2K citations

Ocean University of China
Qingdao, China
12 h-index
51 publications
3.8K citations
Institute of Oceanology
Qingdao, China
12 h-index
32 publications
1.7K citations
NOAA Pacific Marine Environmental Laboratory
Seattle, United States
11 h-index
20 publications
1.6K citations
1–8 of 406
39 publications · 2.7K citations
27
h-index
22 publications · 4.1K citations
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JGR · 27 publications · 2.8K citations
20
h-index
25 publications · 1.2K citations
19
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20 publications · 801 citations
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1–5