Current Divergence

Current Divergance is a geophysical phenomenon characterized as a vector field property in ocean surface currents where the horizontal outflow of water from a given region exceeds the inflow, resulting in a net displacement of surface water masses and often inducing upwelling or downwelling effects in the marine boundary layer.

65

Publications

5K

Citations

166

Authors

109

Institutions

Publications per year

2017–2026

5

Authors

166

  1. LL
    L. Lewin

    University of Colorado Boulder, United States

    2 publications · 41 citations

    2

    h-index

  2. JV
    J. V. Eccles

    Space Environment Corporation (United States), United States

    2 publications · 398 citations

    2

    h-index

  3. GH
    G. Haerendel

    Max Planck Institute for Extraterrestrial Physics, Germany

    2 publications · 398 citations

    2

    h-index

  4. BC
    Bertrand Chapron

    Ifremer, France

    2 publications · 80 citations

    2

    h-index

  5. YY
    Yosuke Yamazaki

    GFZ Helmholtz Centre for Geosciences, Germany

    1 publications · 20 citations

    1

    h-index

1–5 of 166

Venues

  1. Journal of Geophysical Research Atmospheres

    JGR · 5 publications · 519 citations

    5

    h-index

  2. IEEE Transactions on Magnetics

    4 publications · 144 citations

    4

    h-index

  3. Physical Review Letters

    PRL · 4 publications · 1.8K citations

    4

    h-index

  4. Physical Review

    4 publications · 612 citations

    4

    h-index

  5. Geophysical Research Letters

    3 publications · 163 citations

    3

    h-index

1–5