Wind-driven Overturning

Wind-Driven Overturning is a meridional overturning circulation mechanism distinguished by its primary dependence on surface wind stress to induce large-scale oceanic upwelling and downwelling, thereby shaping the meridional transport of water masses in the upper ocean.

108

Publications

8.1K

Citations

303

Authors

161

Institutions

Publications per year

2017–2026

23

Variants

Wind-driven Meridional Overturning Circulation

Authors

303

  1. JM
    Jochem Marotzke

    Max Planck Institute for Meteorology, Germany

    9 publications · 873 citations

    9

    h-index

  2. WE
    William E. Johns

    University of Miami, United States

    7 publications · 865 citations

    7

    h-index

  3. CS
    Christopher S. Meinen

    NOAA Atlantic Oceanographic and Meteorological Laboratories, United States

    6 publications · 768 citations

    6

    h-index

  4. AM
    Andrew McC. Hogg

    Australian National University, Australia

    5 publications · 415 citations

    5

    h-index

  5. HL
    Harry L. Bryden

    National Oceanography Centre, United Kingdom

    5 publications · 637 citations

    5

    h-index

1–5 of 303

Venues

  1. Journal of Physical Oceanography

    31 publications · 2.9K citations

    24

    h-index

  2. Climate Dynamics

    11 publications · 497 citations

    11

    h-index

  3. Journal of Geophysical Research Oceans

    8 publications · 475 citations

    8

    h-index

  4. Journal of Climate

    7 publications · 711 citations

    7

    h-index

  5. Geophysical Research Letters

    7 publications · 390 citations

    7

    h-index

1–5