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

Authors

569

  1. CS
    Claudia Schmid

    NOAA Atlantic Oceanographic and Meteorological Laboratories, United States

    6 publications · 399 citations

    6

    h-index

  2. YY
    Yuzhu You

    Sydney Institute of Marine Science, Australia

    6 publications · 393 citations

    6

    h-index

  3. WZ
    Walter Zenk

    Christian-Albrechts-Universität zu Kiel, Germany

    5 publications · 377 citations

    5

    h-index

  4. IY
    Ichiro Yasuda

    The University of Tokyo, Japan

    5 publications · 681 citations

    5

    h-index

  5. OB
    Olaf Boebel

    Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung, Germany

    5 publications · 323 citations

    5

    h-index

1–5 of 569

Venues

  1. Journal of Geophysical Research Atmospheres

    JGR · 30 publications · 2.1K citations

    22

    h-index

  2. Journal of Physical Oceanography

    18 publications · 2.1K citations

    17

    h-index

  3. Geophysical Research Letters

    12 publications · 713 citations

    12

    h-index

  4. Paleoceanography

    12 publications · 1.1K citations

    12

    h-index

  5. 9

    h-index

1–5