Unavoidable future increase in West Antarctic ice-shelf melting over the twenty-first century

Ocean-driven melting of floating ice-shelves in the Amundsen Sea is currently the main process controlling Antarctica’s contribution to sea-level rise. Using a regional ocean model, we present a comprehensive suite of future projections of ice-shelf melting in the Amundsen Sea. We find that rapid oc...

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Published in:Nature Climate Change
Main Authors: Naughten, Kaitlin A., Holland, Paul R., De Rydt, Jan
Format: Article in Journal/Newspaper
Language:English
Published: Nature Research 2023
Subjects:
Online Access:http://nora.nerc.ac.uk/id/eprint/534263/
https://nora.nerc.ac.uk/id/eprint/534263/1/s41558-023-01818-x.pdf
https://www.nature.com/articles/s41558-023-01818-x
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spelling ftnerc:oai:nora.nerc.ac.uk:534263 2023-12-24T10:08:05+01:00 Unavoidable future increase in West Antarctic ice-shelf melting over the twenty-first century Naughten, Kaitlin A. Holland, Paul R. De Rydt, Jan 2023-10-23 text http://nora.nerc.ac.uk/id/eprint/534263/ https://nora.nerc.ac.uk/id/eprint/534263/1/s41558-023-01818-x.pdf https://www.nature.com/articles/s41558-023-01818-x en eng Nature Research https://nora.nerc.ac.uk/id/eprint/534263/1/s41558-023-01818-x.pdf Naughten, Kaitlin A. orcid:0000-0001-9475-9162 Holland, Paul R. orcid:0000-0001-8370-289X De Rydt, Jan. 2023 Unavoidable future increase in West Antarctic ice-shelf melting over the twenty-first century. Nature Climate Change. 20, pp. https://doi.org/10.1038/s41558-023-01818-x <https://doi.org/10.1038/s41558-023-01818-x> cc_by_4 Publication - Article PeerReviewed 2023 ftnerc https://doi.org/10.1038/s41558-023-01818-x 2023-11-24T00:03:12Z Ocean-driven melting of floating ice-shelves in the Amundsen Sea is currently the main process controlling Antarctica’s contribution to sea-level rise. Using a regional ocean model, we present a comprehensive suite of future projections of ice-shelf melting in the Amundsen Sea. We find that rapid ocean warming, at approximately triple the historical rate, is likely committed over the twenty-first century, with widespread increases in ice-shelf melting, including in regions crucial for ice-sheet stability. When internal climate variability is considered, there is no significant difference between mid-range emissions scenarios and the most ambitious targets of the Paris Agreement. These results suggest that mitigation of greenhouse gases now has limited power to prevent ocean warming that could lead to the collapse of the West Antarctic Ice Sheet. Article in Journal/Newspaper Amundsen Sea Antarc* Antarctic Ice Sheet Ice Shelf Ice Shelves Natural Environment Research Council: NERC Open Research Archive Antarctic Amundsen Sea West Antarctic Ice Sheet Nature Climate Change 13 11 1222 1228
institution Open Polar
collection Natural Environment Research Council: NERC Open Research Archive
op_collection_id ftnerc
language English
description Ocean-driven melting of floating ice-shelves in the Amundsen Sea is currently the main process controlling Antarctica’s contribution to sea-level rise. Using a regional ocean model, we present a comprehensive suite of future projections of ice-shelf melting in the Amundsen Sea. We find that rapid ocean warming, at approximately triple the historical rate, is likely committed over the twenty-first century, with widespread increases in ice-shelf melting, including in regions crucial for ice-sheet stability. When internal climate variability is considered, there is no significant difference between mid-range emissions scenarios and the most ambitious targets of the Paris Agreement. These results suggest that mitigation of greenhouse gases now has limited power to prevent ocean warming that could lead to the collapse of the West Antarctic Ice Sheet.
format Article in Journal/Newspaper
author Naughten, Kaitlin A.
Holland, Paul R.
De Rydt, Jan
spellingShingle Naughten, Kaitlin A.
Holland, Paul R.
De Rydt, Jan
Unavoidable future increase in West Antarctic ice-shelf melting over the twenty-first century
author_facet Naughten, Kaitlin A.
Holland, Paul R.
De Rydt, Jan
author_sort Naughten, Kaitlin A.
title Unavoidable future increase in West Antarctic ice-shelf melting over the twenty-first century
title_short Unavoidable future increase in West Antarctic ice-shelf melting over the twenty-first century
title_full Unavoidable future increase in West Antarctic ice-shelf melting over the twenty-first century
title_fullStr Unavoidable future increase in West Antarctic ice-shelf melting over the twenty-first century
title_full_unstemmed Unavoidable future increase in West Antarctic ice-shelf melting over the twenty-first century
title_sort unavoidable future increase in west antarctic ice-shelf melting over the twenty-first century
publisher Nature Research
publishDate 2023
url http://nora.nerc.ac.uk/id/eprint/534263/
https://nora.nerc.ac.uk/id/eprint/534263/1/s41558-023-01818-x.pdf
https://www.nature.com/articles/s41558-023-01818-x
geographic Antarctic
Amundsen Sea
West Antarctic Ice Sheet
geographic_facet Antarctic
Amundsen Sea
West Antarctic Ice Sheet
genre Amundsen Sea
Antarc*
Antarctic
Ice Sheet
Ice Shelf
Ice Shelves
genre_facet Amundsen Sea
Antarc*
Antarctic
Ice Sheet
Ice Shelf
Ice Shelves
op_relation https://nora.nerc.ac.uk/id/eprint/534263/1/s41558-023-01818-x.pdf
Naughten, Kaitlin A. orcid:0000-0001-9475-9162
Holland, Paul R. orcid:0000-0001-8370-289X
De Rydt, Jan. 2023 Unavoidable future increase in West Antarctic ice-shelf melting over the twenty-first century. Nature Climate Change. 20, pp. https://doi.org/10.1038/s41558-023-01818-x <https://doi.org/10.1038/s41558-023-01818-x>
op_rights cc_by_4
op_doi https://doi.org/10.1038/s41558-023-01818-x
container_title Nature Climate Change
container_volume 13
container_issue 11
container_start_page 1222
op_container_end_page 1228
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