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Sea-ice-driven shallow overturning

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A Correction to this article was published on 29 July 2016

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Conversion of Antarctic circumpolar upwelling waters to less dense water has mainly been attributed to surface heat fluxes. An analysis of water-mass transformation shows that the dominant process is the formation of sea ice near Antarctica and its melt offshore.

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Figure 1: A view of sea ice from the RV Aurora Australis.

Change history

  • 05 July 2016

    In the version of this News and Views originally published online, the wording of the standfirst and the sentence in the first paragraph beginning 'The common view has been...' was potentially misleading. This has now been edited in all versions of the News and Views to better reflect the intended meaning

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Authors and Affiliations

  1. Nathaniel L. Bindoff and William R. Hobbs are at the ARC Centre of Excellence for Climate System Science, UNSW Sydney, New South Wales 2052, Australia and at the Antarctic Climate and Ecosystems Cooperative Research Centre, Private Bag 80, University of Tasmania, Hobart, Tasmania 7001, Australia,

    Nathaniel L. Bindoff & William R. Hobbs

  2. Nathaniel L. Bindoff is also at IMAS, University of Tasmania, Sandy Bay, TAS 7005, Australia and at CSIRO Marine and Atmospheric Research, Hobart, TAS 7000, Australia,

    Nathaniel L. Bindoff

Authors
  1. Nathaniel L. Bindoff
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  2. William R. Hobbs
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Corresponding authors

Correspondence to Nathaniel L. Bindoff or William R. Hobbs.

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Bindoff, N., Hobbs, W. Sea-ice-driven shallow overturning. Nature Geosci 9, 569–570 (2016). https://doi.org/10.1038/ngeo2766

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