Frontal Circulations

Frontal Circulations is a dynamical oceanic process characterized by coupled cross-frontal exchange flows and secondary circulation cells that emerge at density gradients along oceanic fronts, driven by geostrophic and thermal wind imbalances, and distinct from larger-scale basin circulations or local turbulent mixing.

102

Publications

4.9K

Citations

269

Authors

140

Institutions

Publications per year

2017–2026

14

Authors

269

  1. DK
    Daniel Keyser

    University at Albany, State University of New York, United States

    5 publications · 461 citations

    5

    h-index

  2. JC
    James C. McWilliams

    University of California, Los Angeles, United States

    5 publications · 165 citations

    5

    h-index

  3. RW
    Richard W. Garvine

    University of Delaware, United States

    4 publications · 77 citations

    4

    h-index

  4. DL
    Daniel L. Rudnick

    Scripps Institution of Oceanography, United States

    4 publications · 107 citations

    4

    h-index

  5. EP
    Enric Pallàs‐Sanz

    Centro de Investigación Científica y de Educación Superior de Ensenada, Mexico

    3 publications · 101 citations

    3

    h-index

1–5 of 269

Venues

  1. Journal of Physical Oceanography

    13 publications · 463 citations

    13

    h-index

  2. 11

    h-index

  3. Monthly Weather Review

    10 publications · 443 citations

    10

    h-index

  4. Journal of the Atmospheric Sciences

    9 publications · 638 citations

    9

    h-index

  5. Journal of Geophysical Research Atmospheres

    JGR · 9 publications · 387 citations

    9

    h-index

1–5