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Observed interannual changes beneath Filchner-Ronne Ice Shelf linked to large-scale atmospheric circulation

Author

Listed:
  • Tore Hattermann

    (Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research
    Akvaplan-niva AS
    Norwegian Polar Institute)

  • Keith W. Nicholls

    (British Antarctic Survey BAS)

  • Hartmut H. Hellmer

    (Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research)

  • Peter E. D. Davis

    (British Antarctic Survey BAS)

  • Markus A. Janout

    (Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research)

  • Svein Østerhus

    (NORCE Norwegian Research Centre and Bjerknes Centre for Climate Research)

  • Elisabeth Schlosser

    (University of Innsbruck
    Austrian Polar Research Institute)

  • Gerd Rohardt

    (Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research)

  • Torsten Kanzow

    (Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research
    Bremen University, Department of Physics and Electrical Engineering)

Abstract

Floating ice shelves are the Achilles’ heel of the Antarctic Ice Sheet. They limit Antarctica’s contribution to global sea level rise, yet they can be rapidly melted from beneath by a warming ocean. At Filchner-Ronne Ice Shelf, a decline in sea ice formation may increase basal melt rates and accelerate marine ice sheet mass loss within this century. However, the understanding of this tipping-point behavior largely relies on numerical models. Our new multi-annual observations from five hot-water drilled boreholes through Filchner-Ronne Ice Shelf show that since 2015 there has been an intensification of the density-driven ice shelf cavity-wide circulation in response to reinforced wind-driven sea ice formation in the Ronne polynya. Enhanced southerly winds over Ronne Ice Shelf coincide with westward displacements of the Amundsen Sea Low position, connecting the cavity circulation with changes in large-scale atmospheric circulation patterns as a new aspect of the atmosphere-ocean-ice shelf system.

Suggested Citation

  • Tore Hattermann & Keith W. Nicholls & Hartmut H. Hellmer & Peter E. D. Davis & Markus A. Janout & Svein Østerhus & Elisabeth Schlosser & Gerd Rohardt & Torsten Kanzow, 2021. "Observed interannual changes beneath Filchner-Ronne Ice Shelf linked to large-scale atmospheric circulation," Nature Communications, Nature, vol. 12(1), pages 1-11, December.
  • Handle: RePEc:nat:natcom:v:12:y:2021:i:1:d:10.1038_s41467-021-23131-x
    DOI: 10.1038/s41467-021-23131-x
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    Cited by:

    1. H. W. Yang & T.-W. Kim & Pierre Dutrieux & A. K. Wåhlin & Adrian Jenkins & H. K. Ha & C. S. Kim & K.-H. Cho & T. Park & S. H. Lee & Y.-K. Cho, 2022. "Seasonal variability of ocean circulation near the Dotson Ice Shelf, Antarctica," Nature Communications, Nature, vol. 13(1), pages 1-11, December.

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