Upper Ocean Currents

Upper Ocean Currents is a physical oceanographic phenomenon characterized by the horizontal movement of seawater within the upper layer of the ocean, typically extending from the surface down to depths of approximately 100 to 200 meters, driven primarily by wind stress, buoyancy forces, and the Coriolis effect, and distinguished from deeper ocean currents by its strong interaction with atmospheric forcing and its central role in the transfer of heat, momentum, and mass within the ocean–atmosphere system.

325

Publications

21.3K

Citations

1K

Authors

341

Institutions

Publications per year

2017–2026

56

Authors

1K

  1. CC
    Charles C. Eriksen

    University of Washington, United States

    6 publications · 401 citations

    6

    h-index

  2. BL
    Bernard Le Cann

    Centre National de la Recherche Scientifique, France

    6 publications · 870 citations

    6

    h-index

  3. JC
    James C. McWilliams

    University of California, Los Angeles, United States

    6 publications · 625 citations

    6

    h-index

  4. DW
    Dongxiao Wang

    South China Sea Institute Of Oceanology, China

    6 publications · 293 citations

    6

    h-index

  5. TD
    Tommy D. Dickey

    University of California, Santa Barbara, United States

    6 publications · 490 citations

    6

    h-index

1–5 of 1K

Venues

  1. Journal of Physical Oceanography

    55 publications · 4.5K citations

    33

    h-index

  2. Journal of Geophysical Research Atmospheres

    JGR · 50 publications · 3K citations

    30

    h-index

  3. Geophysical Research Letters

    24 publications · 1.7K citations

    19

    h-index

  4. Journal of Geophysical Research Oceans

    19 publications · 689 citations

    16

    h-index

  5. 14

    h-index

1–5