Wind-driven Equatorial Circulation

Wind-Driven Equatorial Circulation is a theoretical framework within equatorial oceanography that describes the large-scale, wind-forced movement of surface and subsurface waters along the equatorial band, distinguished by its dependence on zonal wind stress and the resulting dynamical balance involving the Coriolis effect and pressure gradients.

92

Publications

5.6K

Citations

233

Authors

117

Institutions

Publications per year

2017–2026

10

Authors

233

  1. JP
    Julian P. McCreary

    University of Hawaiʻi at Mānoa, United States

    6 publications · 1K citations

    6

    h-index

  2. SG
    S. George Philander

    Princeton University, United States

    4 publications · 338 citations

    4

    h-index

  3. SH
    Stefan Hastenrath

    University of Wisconsin–Madison, United States

    4 publications · 186 citations

    4

    h-index

  4. SX
    Shang‐Ping Xie

    Scripps Institution of Oceanography, United States

    3 publications · 387 citations

    3

    h-index

  5. RR
    R. Raghavarao

    Physical Research Laboratory, India

    3 publications · 175 citations

    3

    h-index

1–5 of 233

Venues

  1. Journal of Physical Oceanography

    17 publications · 1.4K citations

    16

    h-index

  2. Journal of Geophysical Research Atmospheres

    JGR · 10 publications · 693 citations

    10

    h-index

  3. Geophysical Research Letters

    5 publications · 219 citations

    5

    h-index

  4. Icarus

    5 publications · 209 citations

    5

    h-index

  5. Climate Dynamics

    4 publications · 390 citations

    4

    h-index

1–5