Wind-driven Surface Transport

Wind-Driven Surface Transport is a geophysical fluid dynamics process that constitutes the net movement of surface ocean water in the uppermost layer of the ocean, distinguished by its direct response to wind stress and adherence to Ekman theory, in which the resultant transport occurs at a 90° angle relative to the direction of the prevailing wind due to the Coriolis effect.

86

Publications

4.8K

Citations

301

Authors

152

Institutions

Publications per year

2017–2026

9

Authors

301

  1. TS
    Tarmo Soomere

    Tallinn University of Technology, Estonia

    4 publications · 123 citations

    4

    h-index

  2. ND
    Nicole Delpeche‐Ellmann

    Tallinn University of Technology, Estonia

    3 publications · 88 citations

    3

    h-index

  3. CM
    Cheryl McKenna Neuman

    Trent University, Canada

    3 publications · 240 citations

    3

    h-index

  4. KA
    Knut Aagaard

    University of Washington, United States

    2 publications · 71 citations

    2

    h-index

  5. KM
    Kai Myrberg

    Finnish Environment Institute, Finland

    2 publications · 76 citations

    2

    h-index

1–5 of 301

Venues

  1. Journal of Geophysical Research Atmospheres

    JGR · 14 publications · 522 citations

    12

    h-index

  2. Journal of Physical Oceanography

    6 publications · 397 citations

    6

    h-index

  3. Journal of Marine Systems

    6 publications · 199 citations

    6

    h-index

  4. Continental Shelf Research

    5 publications · 272 citations

    5

    h-index

  5. Geophysical Research Letters

    4 publications · 286 citations

    4

    h-index

1–5