Polynya Convection

Polynya Convection is a polar oceanographic process in which localized, persistent openings in sea ice—polynyas—facilitate intense vertical mixing of ocean water through brine rejection and thermal cooling, thereby driving deep convective overturning in polar marine environments.

31

Publications

1.5K

Citations

81

Authors

51

Institutions

Publications per year

2017–2026

4

Authors

81

  1. AL
    Arnold L. Gordon

    Lamont-Doherty Earth Observatory, United States

    3 publications · 361 citations

    3

    h-index

  2. IA
    Ian A. Renfrew

    University of East Anglia, United Kingdom

    3 publications · 133 citations

    3

    h-index

  3. TG
    Tor Gammelsrød

    University of Bergen, Norway

    2 publications · 75 citations

    2

    h-index

  4. DM
    David M. Holland

    New York University, United States

    2 publications · 129 citations

    2

    h-index

  5. TT
    Tor Tørresen

    University of Bergen, Norway

    2 publications · 75 citations

    2

    h-index

1–5 of 81

Venues

  1. Journal of Physical Oceanography

    4 publications · 340 citations

    4

    h-index

  2. Journal of Geophysical Research Atmospheres

    JGR · 4 publications · 206 citations

    4

    h-index

  3. Polar Research

    3 publications · 109 citations

    3

    h-index

  4. Boundary-Layer Meteorology

    3 publications · 112 citations

    3

    h-index

  5. Tellus A Dynamic Meteorology and Oceanography

    2 publications · 62 citations

    2

    h-index

1–5