West Antarctic Ice Sheet retreat in the Amundsen Sea driven by decadal oceanic variability

Mass loss from the Amundsen Sea sector of the West Antarctic Ice Sheet has increased in recent decades, suggestive of sustained ocean forcing or an ongoing, possibly unstable, response to a past climate anomaly. Lengthening satellite records appear to be incompatible with either process, however, re...

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Published in:Nature Geoscience
Main Authors: Jenkins, Adrian, Shoosmith, Deb, Dutrieux, Pierre, Jacobs, Stan, Kim, Tae Wan, Lee, Sang Hoon, Ha, Ho Kyung, Stammerjohn, Sharon
Format: Article in Journal/Newspaper
Language:English
Published: Springer Nature 2018
Subjects:
Online Access:http://nora.nerc.ac.uk/id/eprint/518311/
https://nora.nerc.ac.uk/id/eprint/518311/1/Jenkins_et_al_Nature_Geoscience_2018%20%28002%29.pdf
http://www.nature.com/articles/s41561-018-0207-4
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spelling ftnerc:oai:nora.nerc.ac.uk:518311 2023-05-15T13:23:40+02:00 West Antarctic Ice Sheet retreat in the Amundsen Sea driven by decadal oceanic variability Jenkins, Adrian Shoosmith, Deb Dutrieux, Pierre Jacobs, Stan Kim, Tae Wan Lee, Sang Hoon Ha, Ho Kyung Stammerjohn, Sharon 2018-10 text http://nora.nerc.ac.uk/id/eprint/518311/ https://nora.nerc.ac.uk/id/eprint/518311/1/Jenkins_et_al_Nature_Geoscience_2018%20%28002%29.pdf http://www.nature.com/articles/s41561-018-0207-4 en eng Springer Nature https://nora.nerc.ac.uk/id/eprint/518311/1/Jenkins_et_al_Nature_Geoscience_2018%20%28002%29.pdf Jenkins, Adrian orcid:0000-0002-9117-0616 Shoosmith, Deb; Dutrieux, Pierre; Jacobs, Stan; Kim, Tae Wan; Lee, Sang Hoon; Ha, Ho Kyung; Stammerjohn, Sharon. 2018 West Antarctic Ice Sheet retreat in the Amundsen Sea driven by decadal oceanic variability. Nature Geoscience, 11 (10). 733-738. https://doi.org/10.1038/s41561-018-0207-4 <https://doi.org/10.1038/s41561-018-0207-4> Publication - Article PeerReviewed 2018 ftnerc https://doi.org/10.1038/s41561-018-0207-4 2023-02-04T19:45:35Z Mass loss from the Amundsen Sea sector of the West Antarctic Ice Sheet has increased in recent decades, suggestive of sustained ocean forcing or an ongoing, possibly unstable, response to a past climate anomaly. Lengthening satellite records appear to be incompatible with either process, however, revealing both periodic hiatuses in acceleration and intermittent episodes of thinning. Here we use ocean temperature, salinity, dissolved-oxygen and current measurements taken from 2000 to 2016 near the Dotson Ice Shelf to determine temporal changes in net basal melting. A decadal cycle dominates the ocean record, with melt changing by a factor of about four between cool and warm extremes via a nonlinear relationship with ocean temperature. A warm phase that peaked around 2009 coincided with ice-shelf thinning and retreat of the grounding line, which re-advanced during a post-2011 cool phase. These observations demonstrate how discontinuous ice retreat is linked with ocean variability, and that the strength and timing of decadal extremes is more influential than changes in the longer-term mean state. The nonlinear response of melting to temperature change heightens the sensitivity of Amundsen Sea ice shelves to such variability, possibly explaining the vulnerability of the ice sheet in that sector, where subsurface ocean temperatures are relatively high. Article in Journal/Newspaper Amundsen Sea Antarc* Antarctic Dotson Ice Shelf Ice Sheet Ice Shelf Ice Shelves Sea ice Natural Environment Research Council: NERC Open Research Archive Antarctic Amundsen Sea West Antarctic Ice Sheet Dotson Ice Shelf ENVELOPE(-112.367,-112.367,-74.400,-74.400) Nature Geoscience 11 10 733 738
institution Open Polar
collection Natural Environment Research Council: NERC Open Research Archive
op_collection_id ftnerc
language English
description Mass loss from the Amundsen Sea sector of the West Antarctic Ice Sheet has increased in recent decades, suggestive of sustained ocean forcing or an ongoing, possibly unstable, response to a past climate anomaly. Lengthening satellite records appear to be incompatible with either process, however, revealing both periodic hiatuses in acceleration and intermittent episodes of thinning. Here we use ocean temperature, salinity, dissolved-oxygen and current measurements taken from 2000 to 2016 near the Dotson Ice Shelf to determine temporal changes in net basal melting. A decadal cycle dominates the ocean record, with melt changing by a factor of about four between cool and warm extremes via a nonlinear relationship with ocean temperature. A warm phase that peaked around 2009 coincided with ice-shelf thinning and retreat of the grounding line, which re-advanced during a post-2011 cool phase. These observations demonstrate how discontinuous ice retreat is linked with ocean variability, and that the strength and timing of decadal extremes is more influential than changes in the longer-term mean state. The nonlinear response of melting to temperature change heightens the sensitivity of Amundsen Sea ice shelves to such variability, possibly explaining the vulnerability of the ice sheet in that sector, where subsurface ocean temperatures are relatively high.
format Article in Journal/Newspaper
author Jenkins, Adrian
Shoosmith, Deb
Dutrieux, Pierre
Jacobs, Stan
Kim, Tae Wan
Lee, Sang Hoon
Ha, Ho Kyung
Stammerjohn, Sharon
spellingShingle Jenkins, Adrian
Shoosmith, Deb
Dutrieux, Pierre
Jacobs, Stan
Kim, Tae Wan
Lee, Sang Hoon
Ha, Ho Kyung
Stammerjohn, Sharon
West Antarctic Ice Sheet retreat in the Amundsen Sea driven by decadal oceanic variability
author_facet Jenkins, Adrian
Shoosmith, Deb
Dutrieux, Pierre
Jacobs, Stan
Kim, Tae Wan
Lee, Sang Hoon
Ha, Ho Kyung
Stammerjohn, Sharon
author_sort Jenkins, Adrian
title West Antarctic Ice Sheet retreat in the Amundsen Sea driven by decadal oceanic variability
title_short West Antarctic Ice Sheet retreat in the Amundsen Sea driven by decadal oceanic variability
title_full West Antarctic Ice Sheet retreat in the Amundsen Sea driven by decadal oceanic variability
title_fullStr West Antarctic Ice Sheet retreat in the Amundsen Sea driven by decadal oceanic variability
title_full_unstemmed West Antarctic Ice Sheet retreat in the Amundsen Sea driven by decadal oceanic variability
title_sort west antarctic ice sheet retreat in the amundsen sea driven by decadal oceanic variability
publisher Springer Nature
publishDate 2018
url http://nora.nerc.ac.uk/id/eprint/518311/
https://nora.nerc.ac.uk/id/eprint/518311/1/Jenkins_et_al_Nature_Geoscience_2018%20%28002%29.pdf
http://www.nature.com/articles/s41561-018-0207-4
long_lat ENVELOPE(-112.367,-112.367,-74.400,-74.400)
geographic Antarctic
Amundsen Sea
West Antarctic Ice Sheet
Dotson Ice Shelf
geographic_facet Antarctic
Amundsen Sea
West Antarctic Ice Sheet
Dotson Ice Shelf
genre Amundsen Sea
Antarc*
Antarctic
Dotson Ice Shelf
Ice Sheet
Ice Shelf
Ice Shelves
Sea ice
genre_facet Amundsen Sea
Antarc*
Antarctic
Dotson Ice Shelf
Ice Sheet
Ice Shelf
Ice Shelves
Sea ice
op_relation https://nora.nerc.ac.uk/id/eprint/518311/1/Jenkins_et_al_Nature_Geoscience_2018%20%28002%29.pdf
Jenkins, Adrian orcid:0000-0002-9117-0616
Shoosmith, Deb; Dutrieux, Pierre; Jacobs, Stan; Kim, Tae Wan; Lee, Sang Hoon; Ha, Ho Kyung; Stammerjohn, Sharon. 2018 West Antarctic Ice Sheet retreat in the Amundsen Sea driven by decadal oceanic variability. Nature Geoscience, 11 (10). 733-738. https://doi.org/10.1038/s41561-018-0207-4 <https://doi.org/10.1038/s41561-018-0207-4>
op_doi https://doi.org/10.1038/s41561-018-0207-4
container_title Nature Geoscience
container_volume 11
container_issue 10
container_start_page 733
op_container_end_page 738
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