Equatorial Upwelling

Equatorial Upwelling is an oceanographic phenomenon characterized by the upward movement of cold, nutrient-rich subsurface waters to the surface layer along the equator, driven primarily by the divergence of surface currents due to zonal wind stress and the Coriolis effect.

278

Publications

25K

Citations

711

Authors

266

Institutions

Publications per year

2017–2026

41

Authors

711

  1. MJ
    Michael J. McPhaden

    NOAA Pacific Marine Environmental Laboratory, United States

    7 publications · 450 citations

    7

    h-index

  2. PB
    Peter Brandt

    GEOMAR Helmholtz Centre for Ocean Research Kiel, Germany

    7 publications · 263 citations

    7

    h-index

  3. RC
    Richard C. Dugdale

    San Francisco State University, United States

    6 publications · 1.1K citations

    6

    h-index

  4. SX
    Shang‐Ping Xie

    Scripps Institution of Oceanography, United States

    6 publications · 411 citations

    6

    h-index

  5. FP
    Frances P. Wilkerson

    San Francisco State University, United States

    6 publications · 1.1K citations

    6

    h-index

1–5 of 711

Venues

  1. Geophysical Research Letters

    35 publications · 2K citations

    27

    h-index

  2. Journal of Geophysical Research Atmospheres

    JGR · 36 publications · 2.2K citations

    27

    h-index

  3. Journal of Physical Oceanography

    31 publications · 2.4K citations

    26

    h-index

  4. Journal of Climate

    25 publications · 3.5K citations

    22

    h-index

  5. Global Biogeochemical Cycles

    13 publications · 1.2K citations

    13

    h-index

1–5