Intermediate Water Circulation
Intermediate Water Circulation is a type of ocean water mass movement characterized by the subsurface flow of water masses occupying mid-ocean depths, typically between 500 and 2000 meters, that are formed by air-sea interactions at subpolar latitudes and distinguished by specific temperature, salinity, and density properties from surface and deep water circulations.
180
Publications
12.9K
Citations
569
Authors
216
Institutions
Publications per year
2017–2026
23
Variants
Intermediate Water Flow
Parents
180
1–5 of 180
569
NOAA Atlantic Oceanographic and Meteorological Laboratories, United States
6 publications · 399 citations
6
h-index
6
h-index
5
h-index
5
h-index
Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung, Germany
5 publications · 323 citations
5
h-index
1–5 of 569
216
The University of Tokyo
Tokyo, Japan
10 h-index
17 publications
1.1K citations
Woods Hole Oceanographic Institution
Falmouth, United States
10 h-index
13 publications
1.3K citations

Centre National de la Recherche Scientifique
Paris, France
10 h-index
33 publications
2K citations

Christian-Albrechts-Universität zu Kiel
Kiel, Germany
7 h-index
14 publications
1.2K citations

Lamont-Doherty Earth Observatory
Sparkill, United States
7 h-index
12 publications
1.9K citations

Scripps Institution of Oceanography
La Jolla, United States
6 h-index
8 publications
1.5K citations
Japan Meteorological Agency
Tokyo, Japan
6 h-index
12 publications
396 citations
Columbia University
New York, United States
6 h-index
12 publications
1.3K citations
1–8 of 216
JGR · 30 publications · 2.1K citations
22
h-index
18 publications · 2.1K citations
17
h-index
12 publications · 713 citations
12
h-index
12 publications · 1.1K citations
12
h-index
9 publications · 850 citations
9
h-index
1–5