Intermediate Water Formation
Intermediate Water Formation is the oceanographic process by which water masses of distinct temperature and salinity characteristics are created at intermediate depths, typically below the surface mixed layer and above the deep ocean, through cooling, evaporation, or mixing processes that increase density and drive subsidence, thereby contributing to the ventilation and stratification of the mid-level ocean circulation.
325
Publications
21K
Citations
950
Authors
343
Institutions
Publications per year
2017–2026
65
325
On the North Atlantic Circulation
William J. Schmitz, Michael S. McCartney · Reviews of Geophysics · 1993 · 754 citations
1–5 of 325
950
16
h-index
11
h-index
11
h-index
8
h-index
7
h-index
1–5 of 950
343
The University of Tokyo
Tokyo, Japan
15 h-index
24 publications
1.1K citations

Centre National de la Recherche Scientifique
Paris, France
15 h-index
33 publications
1.7K citations
Woods Hole Oceanographic Institution
Falmouth, United States
14 h-index
25 publications
1.3K citations

Scripps Institution of Oceanography
La Jolla, United States
13 h-index
27 publications
3K citations
Japan Fisheries Research and Education Agency
Yokohama, Japan
12 h-index
27 publications
1.9K citations
Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung
Bremerhaven, Germany
12 h-index
33 publications
1.9K citations

National Oceanography Centre
Southampton, United Kingdom
11 h-index
25 publications
1.1K citations

Hokkaido University
Sapporo, Japan
11 h-index
37 publications
1.7K citations
1–8 of 343
JGR · 50 publications · 4K citations
34
h-index
36 publications · 2.8K citations
28
h-index
30 publications · 1.7K citations
23
h-index
16 publications · 1.3K citations
16
h-index
13 publications · 436 citations
12
h-index
1–5