Deep Ocean Circulation Variability
Deep Ocean Circulation Variability is a geophysical phenomenon within ocean circulation dynamics that refers to temporal fluctuations in the velocity, direction, and volume transport of deep-ocean currents driven by variations in density gradients, wind forcing, and large-scale climate modes.
96
Publications
12.1K
Citations
292
Authors
170
Institutions
Publications per year
2017–2026
25
96
1–5 of 96
292
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170
Woods Hole Oceanographic Institution
Falmouth, United States
17 h-index
30 publications
3K citations

Lamont-Doherty Earth Observatory
Sparkill, United States
10 h-index
17 publications
6.1K citations

Scripps Institution of Oceanography
La Jolla, United States
6 h-index
11 publications
398 citations
Columbia University
New York, United States
5 h-index
9 publications
4.9K citations
University of California San Diego
San Diego, United States
5 h-index
10 publications
384 citations
The University of Tokyo
Tokyo, Japan
4 h-index
8 publications
146 citations
University of Washington
Seattle, United States
4 h-index
5 publications
234 citations
Qingdao National Laboratory for Marine Science and Technology
Qingdao, China
4 h-index
12 publications
1K citations
1–8 of 170
8 publications · 5.4K citations
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7 publications · 1.5K citations
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6 publications · 214 citations
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5 publications · 113 citations
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5 publications · 144 citations
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