Mesoscale Eddy Response
Mesoscale Eddy Response is a geophysical process in which oceanic mesoscale eddies, typically 10–100 km in scale, modulate the upper ocean’s thermal, kinetic, and biological properties in reaction to atmospheric forcing or larger-scale flow changes, distinguishing it from broader oceanic responses by its characteristic spatial coherence and rotational dynamics.
397
Publications
26.3K
Citations
1.3K
Authors
386
Institutions
Publications per year
2017–2026
135
Parents
397
Influence of mesoscale eddies on new production in the Sargasso Sea
Dennis J. McGillicuddy, Allan R. Robinson, David A. Siegel et al. · Nature · 1998 · 1K citations
1–5 of 397
1.3K
9
h-index
Woods Hole Oceanographic Institution, United States
7 publications · 2.2K citations
7
h-index
6
h-index
6
h-index
5
h-index
1–5 of 1.3K
386
Institute of Oceanology
Qingdao, China
21 h-index
126 publications
4.5K citations

University of Hawaiʻi at Mānoa
Honolulu, United States
19 h-index
34 publications
2.8K citations

Scripps Institution of Oceanography
La Jolla, United States
19 h-index
35 publications
2.8K citations

Chinese Academy of Sciences
Beijing, China
19 h-index
112 publications
3.8K citations
Woods Hole Oceanographic Institution
Falmouth, United States
19 h-index
36 publications
5.4K citations
South China Sea Institute Of Oceanology
Guangzhou, China
18 h-index
84 publications
3.2K citations

Centre National de la Recherche Scientifique
Paris, France
17 h-index
63 publications
4.6K citations

Ocean University of China
Qingdao, China
17 h-index
64 publications
3.4K citations
1–8 of 386
41 publications · 2.9K citations
29
h-index
32 publications · 2.7K citations
25
h-index
23 publications · 1.5K citations
22
h-index
JGR · 35 publications · 1.9K citations
22
h-index
21 publications · 1.2K citations
18
h-index
1–5