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Storm-induced sea-ice breakup and the implications for ice extent

Author

Listed:
  • A. L. Kohout

    (National Institute of Water and Atmospheric Research, Christchurch 8011, New Zealand)

  • M. J. M. Williams

    (National Institute of Water and Atmospheric Research, Wellington 6021, New Zealand)

  • S. M. Dean

    (National Institute of Water and Atmospheric Research, Wellington 6021, New Zealand)

  • M. H. Meylan

    (The University of Newcastle, Newcastle, New South Wales 2308, Australia)

Abstract

Concurrent observations at multiple locations indicate that storm-generated ocean waves propagating through Antarctic sea ice can transport enough energy to break first-year sea ice hundreds of kilometres from the ice edge, which is much farther than would be predicted by the commonly assumed exponential wave decay.

Suggested Citation

  • A. L. Kohout & M. J. M. Williams & S. M. Dean & M. H. Meylan, 2014. "Storm-induced sea-ice breakup and the implications for ice extent," Nature, Nature, vol. 509(7502), pages 604-607, May.
  • Handle: RePEc:nat:nature:v:509:y:2014:i:7502:d:10.1038_nature13262
    DOI: 10.1038/nature13262
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    Cited by:

    1. Alberto Alberello & Luke G. Bennetts & Miguel Onorato & Marcello Vichi & Keith MacHutchon & Clare Eayrs & Butteur Ntamba Ntamba & Alvise Benetazzo & Filippo Bergamasco & Filippo Nelli & Rohinee Pattan, 2022. "Three-dimensional imaging of waves and floes in the marginal ice zone during a cyclone," Nature Communications, Nature, vol. 13(1), pages 1-11, December.

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