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Linear sea-level response to abrupt ocean warming of major West Antarctic ice basin

Author

Listed:
  • M. Mengel

    (Potsdam Institute for Climate Impact Research
    Institute of Physics, Potsdam University)

  • J. Feldmann

    (Potsdam Institute for Climate Impact Research
    Institute of Physics, Potsdam University)

  • A. Levermann

    (Potsdam Institute for Climate Impact Research
    Institute of Physics, Potsdam University)

Abstract

Ice shelves lose ice through both melting caused by warm marine waters and instability. For the Filchner–Ronne ice shelf, West Antarctica, ice loss is dominated by melt due to warm water intrusion, rather than marine ice-sheet instability.

Suggested Citation

  • M. Mengel & J. Feldmann & A. Levermann, 2016. "Linear sea-level response to abrupt ocean warming of major West Antarctic ice basin," Nature Climate Change, Nature, vol. 6(1), pages 71-74, January.
    • Handle: RePEc:nat:natcli:v:6:y:2016:i:1:d:10.1038_nclimate2808
    DOI: 10.1038/nclimate2808
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