Increased warm water intrusions could cause mass loss in East Antarctica during the next 200 years

The East Antarctic Ice Sheet is currently surrounded by relatively cool water but changes in ocean dynamics may lead to warmer ocean water on the shelf in the future. This has the potential to dramatically increase its future sea level contribution.

Bibliographic Details
Published in:Nature Communications
Main Authors: James R. Jordan, B. W. J. Miles, G. H. Gudmundsson, S. S. R. Jamieson, A. Jenkins, C. R. Stokes
Format: Article in Journal/Newspaper
Language:English
Published: Nature Portfolio 2023
Subjects:
Science
Q
Antarctic
East Antarctic Ice Sheet
East Antarctica
Antarc*
Antarctica
Ice Sheet
Online Access:https://doi.org/10.1038/s41467-023-37553-2
https://doaj.org/article/7fb4a2a2d972401698a3ab2887a2c096
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spelling ftdoajarticles:oai:doaj.org/article:7fb4a2a2d972401698a3ab2887a2c096 2023-05-15T14:02:52+02:00 Increased warm water intrusions could cause mass loss in East Antarctica during the next 200 years James R. Jordan B. W. J. Miles G. H. Gudmundsson S. S. R. Jamieson A. Jenkins C. R. Stokes 2023-04-01T00:00:00Z https://doi.org/10.1038/s41467-023-37553-2 https://doaj.org/article/7fb4a2a2d972401698a3ab2887a2c096 EN eng Nature Portfolio https://doi.org/10.1038/s41467-023-37553-2 https://doaj.org/toc/2041-1723 doi:10.1038/s41467-023-37553-2 2041-1723 https://doaj.org/article/7fb4a2a2d972401698a3ab2887a2c096 Nature Communications, Vol 14, Iss 1, Pp 1-11 (2023) Science Q article 2023 ftdoajarticles https://doi.org/10.1038/s41467-023-37553-2 2023-04-09T00:35:19Z The East Antarctic Ice Sheet is currently surrounded by relatively cool water but changes in ocean dynamics may lead to warmer ocean water on the shelf in the future. This has the potential to dramatically increase its future sea level contribution. Article in Journal/Newspaper Antarc* Antarctic Antarctica East Antarctica Ice Sheet Directory of Open Access Journals: DOAJ Articles Antarctic East Antarctic Ice Sheet East Antarctica Nature Communications 14 1
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Science
Q
spellingShingle Science
Q
James R. Jordan
B. W. J. Miles
G. H. Gudmundsson
S. S. R. Jamieson
A. Jenkins
C. R. Stokes
Increased warm water intrusions could cause mass loss in East Antarctica during the next 200 years
topic_facet Science
Q
description The East Antarctic Ice Sheet is currently surrounded by relatively cool water but changes in ocean dynamics may lead to warmer ocean water on the shelf in the future. This has the potential to dramatically increase its future sea level contribution.
format Article in Journal/Newspaper
author James R. Jordan
B. W. J. Miles
G. H. Gudmundsson
S. S. R. Jamieson
A. Jenkins
C. R. Stokes
author_facet James R. Jordan
B. W. J. Miles
G. H. Gudmundsson
S. S. R. Jamieson
A. Jenkins
C. R. Stokes
author_sort James R. Jordan
title Increased warm water intrusions could cause mass loss in East Antarctica during the next 200 years
title_short Increased warm water intrusions could cause mass loss in East Antarctica during the next 200 years
title_full Increased warm water intrusions could cause mass loss in East Antarctica during the next 200 years
title_fullStr Increased warm water intrusions could cause mass loss in East Antarctica during the next 200 years
title_full_unstemmed Increased warm water intrusions could cause mass loss in East Antarctica during the next 200 years
title_sort increased warm water intrusions could cause mass loss in east antarctica during the next 200 years
publisher Nature Portfolio
publishDate 2023
url https://doi.org/10.1038/s41467-023-37553-2
https://doaj.org/article/7fb4a2a2d972401698a3ab2887a2c096
geographic Antarctic
East Antarctic Ice Sheet
East Antarctica
geographic_facet Antarctic
East Antarctic Ice Sheet
East Antarctica
genre Antarc*
Antarctic
Antarctica
East Antarctica
Ice Sheet
genre_facet Antarc*
Antarctic
Antarctica
East Antarctica
Ice Sheet
op_source Nature Communications, Vol 14, Iss 1, Pp 1-11 (2023)
op_relation https://doi.org/10.1038/s41467-023-37553-2
https://doaj.org/toc/2041-1723
doi:10.1038/s41467-023-37553-2
2041-1723
https://doaj.org/article/7fb4a2a2d972401698a3ab2887a2c096
op_doi https://doi.org/10.1038/s41467-023-37553-2
container_title Nature Communications
container_volume 14
container_issue 1
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