Polynya-driven Upwelling

Polynya-Driven Upwelling is a polar oceanographic process in which localized open-water regions (polynyas) induce vertical ocean circulation through enhanced surface buoyancy loss, leading to the sustained upwelling of deep, dense water masses to the upper ocean.

38

Publications

2.4K

Citations

132

Authors

66

Institutions

Publications per year

2017–2026

3

Authors

132

  1. SK
    Sergey Kirillov

    Arctic and Antarctic Research Institute, Russia

    4 publications · 181 citations

    4

    h-index

  2. ID
    Igor Dmitrenko

    Arctic and Antarctic Research Institute, Russia

    4 publications · 181 citations

    4

    h-index

  3. JH
    Jens Hölemann

    Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung, Germany

    4 publications · 200 citations

    4

    h-index

  4. GB
    Gereon Budéus

    Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung, Germany

    3 publications · 105 citations

    3

    h-index

  5. HE
    Hajo Eicken

    University of Alaska Fairbanks, United States

    3 publications · 136 citations

    3

    h-index

1–5 of 132

Venues

  1. Journal of Geophysical Research Atmospheres

    JGR · 7 publications · 917 citations

    7

    h-index

  2. Journal of Marine Systems

    5 publications · 142 citations

    5

    h-index

  3. Polar Biology

    3 publications · 229 citations

    3

    h-index

  4. Journal of Geophysical Research Oceans

    3 publications · 108 citations

    3

    h-index

  5. Progress In Oceanography

    2 publications · 132 citations

    2

    h-index

1–5