Front-associated Eddies

Front-Associated Eddies is a hydrodynamic phenomenon denoting a mesoscale coherent vortex structure that forms, persists, or intensifies in the vicinity of an ocean front due to baroclinic instability, shear instability, or frontogenetic processes, thereby mediating cross-frontal exchanges of heat, nutrients, and momentum.

27

Publications

2.5K

Citations

89

Authors

54

Institutions

Publications per year

2017–2026

5

Authors

89

  1. JS
    Justin Small

    NSF National Center for Atmospheric Research, United States

    2 publications · 921 citations

    2

    h-index

  2. JG
    Jonathan Gula

    Centre National de la Recherche Scientifique, France

    2 publications · 159 citations

    2

    h-index

  3. PF
    P. F. Linden

    University of Cambridge, United Kingdom

    2 publications · 180 citations

    2

    h-index

  4. CM
    Claire Ménesguen

    Ifremer, France

    2 publications · 101 citations

    2

    h-index

  5. DC
    David Chapman

    Woods Hole Oceanographic Institution, United States

    2 publications · 93 citations

    2

    h-index

1–5 of 89

Venues

  1. Journal of Physical Oceanography

    5 publications · 248 citations

    5

    h-index

  2. Journal of Geophysical Research Atmospheres

    JGR · 3 publications · 123 citations

    3

    h-index

  3. 3

    h-index

  4. 2

    h-index

  5. Dynamics of Atmospheres and Oceans

    2 publications · 925 citations

    2

    h-index

1–5