Downwelling Currents

Downwelling Currents is a surface current phenomenon characterized by the downward movement of surface water due to convergence of horizontal currents, typically driven by wind stress and Coriolis forces, resulting in the transport of warm, oxygen-rich surface water to deeper ocean layers.

42

Publications

1.9K

Citations

113

Authors

64

Institutions

Publications per year

2017–2026

4

Authors

113

  1. PP
    Pearn P. Niiler

    Scripps Institution of Oceanography, United States

    2 publications · 40 citations

    2

    h-index

  2. WJ
    William J. Schmitz

    Woods Hole Oceanographic Institution, United States

    2 publications · 40 citations

    2

    h-index

  3. FC
    F. C. Fuglister

    Woods Hole Oceanographic Institution, United States

    2 publications · 54 citations

    2

    h-index

  4. TT
    Toshihiko Teramoto

    The University of Tokyo, Japan

    2 publications · 47 citations

    2

    h-index

  5. RP
    Ricardo P. Matano

    Oregon State University, United States

    1 publications · 125 citations

    1

    h-index

1–5 of 113

Venues

  1. Journal of Physical Oceanography

    8 publications · 445 citations

    8

    h-index

  2. Journal of Geophysical Research Atmospheres

    JGR · 6 publications · 233 citations

    6

    h-index

  3. Continental Shelf Research

    3 publications · 90 citations

    3

    h-index

  4. Journal of Oceanography

    3 publications · 107 citations

    3

    h-index

  5. Journal of Marine Research

    3 publications · 450 citations

    3

    h-index

1–5