Ocean Circulation

Ocean circulation is the large-scale movement of ocean water masses throughout the world's basins, driven by wind stress, internal density gradients, and the Coriolis effect, that functions as the primary mechanism for redistributing heat and carbon globally and regulating Earth's climate.

15.4K

Publications

1.1M

Citations

19.1K

Authors

2.8K

Institutions

Publications per year

2017–2026

2.8K

Authors

19.1K

  1. JC
    James C. McWilliams

    University of California, Los Angeles, United States

    104 publications · 19K citations

    56

    h-index

  2. CW
    Carl Wunsch

    Massachusetts Institute of Technology, United States

    85 publications · 13.7K citations

    51

    h-index

  3. AL
    Arnold L. Gordon

    Lamont-Doherty Earth Observatory, United States

    89 publications · 8.5K citations

    49

    h-index

  4. WE
    William E. Johns

    University of Miami, United States

    75 publications · 8.5K citations

    49

    h-index

  5. RS
    Robert S. Pickart

    Woods Hole Oceanographic Institution, United States

    76 publications · 6K citations

    45

    h-index

1–5 of 19.1K

Venues

  1. Journal of Geophysical Research Atmospheres

    JGR · 2.2K publications · 184.4K citations

    187

    h-index

  2. Journal of Physical Oceanography

    2.4K publications · 175.3K citations

    177

    h-index

  3. Geophysical Research Letters

    1K publications · 68K citations

    124

    h-index

  4. Journal of Climate

    458 publications · 41.4K citations

    106

    h-index

  5. Journal of Geophysical Research Oceans

    1K publications · 46.7K citations

    93

    h-index

1–5

See also

Ocean Circulation

Driving Forces

Major Components

Climate Impacts

Observation Methods

Variability Patterns