Surface Drift

Surface Drift is a geophysical phenomenon denoting the net movement of surface ocean water induced by wind stress and modified by the Coriolis effect, distinguished from deeper current systems by its direct responsiveness to atmospheric forcing and its role in the upper-layer transport of heat, nutrients, and marine debris.

255

Publications

13.2K

Citations

680

Authors

311

Institutions

Publications per year

2017–2026

45

Variants

Surface Current

Authors

680

  1. TM
    Tamay M. Özgökmen

    University of Miami, United States

    5 publications · 605 citations

    5

    h-index

  2. AC
    Andrew C. Poje

    College of Staten Island, United States

    5 publications · 461 citations

    5

    h-index

  3. ML
    Michael L. Banner

    UNSW Sydney, Australia

    4 publications · 547 citations

    4

    h-index

  4. JD
    Jeffrey D. Paduan

    Naval Postgraduate School, United States

    4 publications · 283 citations

    4

    h-index

  5. LH
    L.J.F. Hermans

    Leiden University, Netherlands

    4 publications · 85 citations

    4

    h-index

1–5 of 680

Venues

  1. Journal of Physical Oceanography

    27 publications · 1.4K citations

    19

    h-index

  2. Journal of Geophysical Research Atmospheres

    JGR · 20 publications · 1.9K citations

    18

    h-index

  3. Geophysical Research Letters

    12 publications · 619 citations

    12

    h-index

  4. Journal of Fluid Mechanics

    11 publications · 1.3K citations

    11

    h-index

  5. 6

    h-index

1–5