Oceanic Ekman Layer

Oceanic Ekman Layer is a theoretical boundary layer in geophysical fluid dynamics that describes the vertical structure of wind-driven ocean currents in the upper ocean, distinguished by a balance between the Coriolis force, vertical eddy viscosity, and applied wind stress, resulting in a characteristic spiral of current velocity with depth.

145

Publications

8K

Citations

337

Authors

145

Institutions

Publications per year

2017–2026

16

Authors

337

  1. GW
    Gareth Williams

    NOAA Geophysical Fluid Dynamics Laboratory, United States

    3 publications · 99 citations

    3

    h-index

  2. MA
    Michael A. Spall

    Woods Hole Oceanographic Institution, United States

    3 publications · 82 citations

    3

    h-index

  3. JC
    James C. McWilliams

    University of California, Los Angeles, United States

    3 publications · 212 citations

    3

    h-index

  4. JP
    Joseph Pedlosky

    Woods Hole Oceanographic Institution, United States

    3 publications · 131 citations

    3

    h-index

  5. BG
    Branko Grisogono

    University of Zagreb, Croatia

    3 publications · 124 citations

    3

    h-index

1–5 of 337

Venues

  1. Journal of Physical Oceanography

    37 publications · 2.1K citations

    25

    h-index

  2. Journal of Geophysical Research Atmospheres

    JGR · 16 publications · 774 citations

    15

    h-index

  3. Journal of Fluid Mechanics

    9 publications · 436 citations

    9

    h-index

  4. Journal of Oceanography

    5 publications · 89 citations

    6

    h-index

  5. Journal of the Atmospheric Sciences

    4 publications · 143 citations

    4

    h-index

1–5