Antarctic ice sheet discharge driven by atmosphere-ocean feedbacks at the Last Glacial Termination

Reconstructing the dynamic response of the Antarctic ice sheets to warming during the Last Glacial Termination (LGT; 18,000–11,650 yrs ago) allows us to disentangle ice-climate feedbacks that are key to improving future projections. Whilst the sequence of events during this period is reasonably well...

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Bibliographic Details
Published in:Scientific Reports
Main Authors: Fogwill, CJ, Turney, C, Golledge, NR, Etheridge, DM, Rubino, M, Thornton, DP, Baker, A, Woodward, J, Winter, K, van Ommen, TD, Moy, AD, Curran, MAJ, Davies, SM, Weber, ME, Bird, MI, Munksgaard, NC, Menviel, L, Rootes, CM, Ellis, B, Millman, H, Vohra, J, Rivera, A, Cooper, A
Format: Article in Journal/Newspaper
Language:unknown
Published: Nature Publishing Group: Open Access Journals - Option C 2017
Subjects:
Antarctic
Southern Ocean
The Antarctic
Weddell Sea
Weddell
Antarc*
ice core
Ice Sheet
Online Access:http://hdl.handle.net/1959.4/unsworks_42665
https://unsworks.unsw.edu.au/bitstreams/b247b132-e34e-4e04-b1c7-5b094e9d8f0a/download
https://doi.org/10.1038/srep39979
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Summary:Reconstructing the dynamic response of the Antarctic ice sheets to warming during the Last Glacial Termination (LGT; 18,000–11,650 yrs ago) allows us to disentangle ice-climate feedbacks that are key to improving future projections. Whilst the sequence of events during this period is reasonably well-known, relatively poor chronological control has precluded precise alignment of ice, atmospheric and marine records, making it difficult to assess relationships between Antarctic ice-sheet (AIS) dynamics, climate change and sea level. Here we present results from a highly-resolved ‘horizontal ice core’ from the Weddell Sea Embayment, which records millennial-scale AIS dynamics across this extensive region. Counterintuitively, we find AIS mass-loss across the full duration of the Antarctic Cold Reversal (ACR; 14,600–12,700 yrs ago), with stabilisation during the subsequent millennia of atmospheric warming. Earth-system and ice-sheet modelling suggests these contrasting trends were likely Antarctic-wide, sustained by feedbacks amplified by the delivery of Circumpolar Deep Water onto the continental shelf. Given the anti-phase relationship between inter-hemispheric climate trends across the LGT our findings demonstrate that Southern Ocean-AIS feedbacks were controlled by global atmospheric teleconnections. With increasing stratification of the Southern Ocean and intensification of mid-latitude westerly winds today, such teleconnections could amplify AIS mass loss and accelerate global sea-level rise.

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