Large-scale Wind-driven Circulation

Large-Scale Wind-Driven Circulation is a theoretical construct in physical oceanography that describes the broad, basin-scale patterns of ocean surface currents generated predominantly by the sustained forcing of global wind stress, distinguished by its geostrophic balance, curl-driven Ekman transport, and role in forming major gyres and western boundary currents.

398

Publications

28.7K

Citations

1.1K

Authors

410

Institutions

Publications per year

2017–2026

64

Authors

1.1K

  1. AM
    Alan M. Davies

    British Oceanographic Data Centre, United Kingdom

    6 publications · 191 citations

    6

    h-index

  2. BQ
    Bo Qiu

    University of Hawaiʻi at Mānoa, United States

    6 publications · 904 citations

    6

    h-index

  3. RX
    Rui Xin Huang

    Woods Hole Oceanographic Institution, United States

    4 publications · 191 citations

    4

    h-index

  4. CW
    Carl Wunsch

    Massachusetts Institute of Technology, United States

    3 publications · 1.2K citations

    3

    h-index

  5. JW
    Jürgen Willebrand

    Christian-Albrechts-Universität zu Kiel, Germany

    3 publications · 525 citations

    3

    h-index

1–5 of 1.1K

Venues

  1. Journal of Physical Oceanography

    53 publications · 4.2K citations

    36

    h-index

  2. Journal of Geophysical Research Atmospheres

    JGR · 39 publications · 2.3K citations

    28

    h-index

  3. Journal of Climate

    19 publications · 1.6K citations

    18

    h-index

  4. Continental Shelf Research

    19 publications · 731 citations

    15

    h-index

  5. Monthly Weather Review

    14 publications · 1.9K citations

    13

    h-index

1–5