Sub-ice-shelf Circulation

Sub-Ice-Shelf Circulation is a glaciological process denoting the movement of oceanic water beneath marine ice shelves, driven by density gradients and tidal forcing, which distinguishes it from other ice-ocean interaction dynamics through its role in regulating basal melt patterns and exchange of heat and freshwater between the continental shelf and the sub-ice-shelf cavity.

108

Publications

9.6K

Citations

369

Authors

160

Institutions

Publications per year

2017–2026

32

Authors

369

  1. AJ
    Adrian Jenkins

    British Antarctic Survey, United Kingdom

    19 publications · 3K citations

    17

    h-index

  2. KW
    Keith W. Nicholls

    British Antarctic Survey, United Kingdom

    14 publications · 853 citations

    14

    h-index

  3. HH
    Hartmut Hellmer

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

    12 publications · 2K citations

    12

    h-index

  4. KM
    Keith Makinson

    British Antarctic Survey, United Kingdom

    11 publications · 707 citations

    11

    h-index

  5. PD
    Pierre Dutrieux

    British Antarctic Survey, United Kingdom

    10 publications · 944 citations

    10

    h-index

1–5 of 369

Venues

  1. Journal of Geophysical Research Oceans

    17 publications · 1.2K citations

    17

    h-index

  2. Journal of Geophysical Research Atmospheres

    JGR · 13 publications · 1.2K citations

    13

    h-index

  3. Journal of Glaciology

    13 publications · 1.2K citations

    12

    h-index

  4. Annals of Glaciology

    6 publications · 622 citations

    6

    h-index

  5. Geophysical Research Letters

    6 publications · 677 citations

    6

    h-index

1–5