Shelf-break Fronts

Shelf-Break Fronts is an oceanic front characterized by a sharp lateral gradient in water properties, such as temperature and salinity, that forms at the boundary between the continental shelf and the deeper ocean, where abrupt topographic change induces baroclinic circulation and mesoscale dynamical processes.

98

Publications

6.4K

Citations

269

Authors

127

Institutions

Publications per year

2017–2026

10

Authors

269

  1. GG
    Glen Gawarkiewicz

    Woods Hole Oceanographic Institution, United States

    16 publications · 879 citations

    14

    h-index

  2. RW
    Robert W. Houghton

    Lamont-Doherty Earth Observatory, United States

    6 publications · 357 citations

    6

    h-index

  3. DC
    David Chapman

    Woods Hole Oceanographic Institution, United States

    4 publications · 218 citations

    4

    h-index

  4. AP
    Alberto Piola

    Argentine Naval Hydrographic Service, Argentina

    4 publications · 450 citations

    4

    h-index

  5. RG
    Raúl Guerrero

    Instituto Nacional de Investigacion y Desarrollo Pesquero, Argentina

    3 publications · 1.2K citations

    3

    h-index

1–5 of 269

Venues

  1. Journal of Geophysical Research Atmospheres

    JGR · 14 publications · 919 citations

    14

    h-index

  2. Journal of Physical Oceanography

    13 publications · 712 citations

    13

    h-index

  3. Continental Shelf Research

    10 publications · 698 citations

    10

    h-index

  4. Geophysical Research Letters

    9 publications · 460 citations

    9

    h-index

  5. Journal of Marine Research

    5 publications · 278 citations

    5

    h-index

1–5