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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ftunivchile:oai:repositorio.uchile.cl:2250/168817 2023-05-15T13:59:14+02:00 Antarctic ice sheet discharge driven by atmosphere-ocean feedbacks at the Last Glacial Termination Fogwill, C. J. Turney, C. S. M. Golledge, N. R. Etheridge, D. M. Rubino, M. Thornton, D. P. Baker, A. Woodward, J. Winter, K. Van Ommen, T. D. Moy, A. D. Curran, M. A. J. Davies, S. M. Weber, M. E. Bird, M. I. Munksgaard, N. C. Menviel, L. Rootes, C. M. Ellis, B. Millman, H. Vohra, J. Rivera, A. Cooper, A. 2017 application/pdf https://doi.org/10.1038/srep39979 https://repositorio.uchile.cl/handle/2250/168817 en eng Nature Scientific Reports, Volumen 7, 2017 20452322 doi:10.1038/srep39979 https://repositorio.uchile.cl/handle/2250/168817 Attribution-NonCommercial-NoDerivs 3.0 Chile http://creativecommons.org/licenses/by-nc-nd/3.0/cl/ CC-BY-NC-ND Scientific Reports Multidisciplinary Artículo de revista 2017 ftunivchile https://doi.org/10.1038/srep39979 2023-01-22T00:56:24Z 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. Article in Journal/Newspaper Antarc* Antarctic ice core Ice Sheet Southern Ocean Weddell Sea Universidad de Chile: Repositorio académico Antarctic Southern Ocean The Antarctic Weddell Weddell Sea Scientific Reports 7 1 |
institution |
Open Polar |
collection |
Universidad de Chile: Repositorio académico |
op_collection_id |
ftunivchile |
language |
English |
topic |
Multidisciplinary |
spellingShingle |
Multidisciplinary Fogwill, C. J. Turney, C. S. M. Golledge, N. R. Etheridge, D. M. Rubino, M. Thornton, D. P. Baker, A. Woodward, J. Winter, K. Van Ommen, T. D. Moy, A. D. Curran, M. A. J. Davies, S. M. Weber, M. E. Bird, M. I. Munksgaard, N. C. Menviel, L. Rootes, C. M. Ellis, B. Millman, H. Vohra, J. Rivera, A. Cooper, A. Antarctic ice sheet discharge driven by atmosphere-ocean feedbacks at the Last Glacial Termination |
topic_facet |
Multidisciplinary |
description |
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. |
format |
Article in Journal/Newspaper |
author |
Fogwill, C. J. Turney, C. S. M. Golledge, N. R. Etheridge, D. M. Rubino, M. Thornton, D. P. Baker, A. Woodward, J. Winter, K. Van Ommen, T. D. Moy, A. D. Curran, M. A. J. Davies, S. M. Weber, M. E. Bird, M. I. Munksgaard, N. C. Menviel, L. Rootes, C. M. Ellis, B. Millman, H. Vohra, J. Rivera, A. Cooper, A. |
author_facet |
Fogwill, C. J. Turney, C. S. M. Golledge, N. R. Etheridge, D. M. Rubino, M. Thornton, D. P. Baker, A. Woodward, J. Winter, K. Van Ommen, T. D. Moy, A. D. Curran, M. A. J. Davies, S. M. Weber, M. E. Bird, M. I. Munksgaard, N. C. Menviel, L. Rootes, C. M. Ellis, B. Millman, H. Vohra, J. Rivera, A. Cooper, A. |
author_sort |
Fogwill, C. J. |
title |
Antarctic ice sheet discharge driven by atmosphere-ocean feedbacks at the Last Glacial Termination |
title_short |
Antarctic ice sheet discharge driven by atmosphere-ocean feedbacks at the Last Glacial Termination |
title_full |
Antarctic ice sheet discharge driven by atmosphere-ocean feedbacks at the Last Glacial Termination |
title_fullStr |
Antarctic ice sheet discharge driven by atmosphere-ocean feedbacks at the Last Glacial Termination |
title_full_unstemmed |
Antarctic ice sheet discharge driven by atmosphere-ocean feedbacks at the Last Glacial Termination |
title_sort |
antarctic ice sheet discharge driven by atmosphere-ocean feedbacks at the last glacial termination |
publisher |
Nature |
publishDate |
2017 |
url |
https://doi.org/10.1038/srep39979 https://repositorio.uchile.cl/handle/2250/168817 |
geographic |
Antarctic Southern Ocean The Antarctic Weddell Weddell Sea |
geographic_facet |
Antarctic Southern Ocean The Antarctic Weddell Weddell Sea |
genre |
Antarc* Antarctic ice core Ice Sheet Southern Ocean Weddell Sea |
genre_facet |
Antarc* Antarctic ice core Ice Sheet Southern Ocean Weddell Sea |
op_source |
Scientific Reports |
op_relation |
Scientific Reports, Volumen 7, 2017 20452322 doi:10.1038/srep39979 https://repositorio.uchile.cl/handle/2250/168817 |
op_rights |
Attribution-NonCommercial-NoDerivs 3.0 Chile http://creativecommons.org/licenses/by-nc-nd/3.0/cl/ |
op_rightsnorm |
CC-BY-NC-ND |
op_doi |
https://doi.org/10.1038/srep39979 |
container_title |
Scientific Reports |
container_volume |
7 |
container_issue |
1 |
_version_ |
1766267744914767872 |