Wind-driven Shelf Circulation

Wind-Driven Shelf Circulation is a large-scale oceanographic circulation pattern on the continental shelf in which the primary driving force is the tangential stress exerted by wind on the sea surface, distinguished by its confinement to shallow, coastal regions and its dynamical balance involving wind forcing, Coriolis effect, and bottom friction.

213

Publications

12.1K

Citations

502

Authors

175

Institutions

Publications per year

2017–2026

20

Authors

502

  1. SJ
    Steven J. Lentz

    Woods Hole Oceanographic Institution, United States

    12 publications · 1.2K citations

    12

    h-index

  2. JS
    J. S. Allen

    Oregon State University, United States

    10 publications · 902 citations

    10

    h-index

  3. RC
    Robert C. Beardsley

    Woods Hole Oceanographic Institution, United States

    7 publications · 567 citations

    7

    h-index

  4. VH
    Vassiliki H. Kourafalou

    University of Miami, United States

    6 publications · 474 citations

    6

    h-index

  5. CD
    Clinton D. Winant

    Scripps Institution of Oceanography, United States

    6 publications · 367 citations

    6

    h-index

1–5 of 502

Venues

  1. Journal of Geophysical Research Atmospheres

    JGR · 50 publications · 3.9K citations

    35

    h-index

  2. Journal of Physical Oceanography

    55 publications · 2.8K citations

    29

    h-index

  3. Continental Shelf Research

    28 publications · 986 citations

    19

    h-index

  4. Geophysical Research Letters

    9 publications · 460 citations

    9

    h-index

  5. Journal of Geophysical Research Oceans

    8 publications · 320 citations

    8

    h-index

1–5