Warming beneath an East Antarctic ice shelf due to increased subpolar westerlies and reduced sea ice

Understanding how climate change influences ocean-driven melting of the Antarctic ice shelves is one of the greatest challenges for projecting future sea level rise. The East Antarctic ice shelf cavities host cold water masses that limit melting, and only a few short-term observational studies exist...

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Published in:Nature Geoscience
Main Authors: Lauber, Julius, Hattermann, Tore, de Steur, Laura, Chiche, Elin Maria Kristina Darelius, Auger, Matthis, Nøst, Ole Anders, Moholdt, Geir
Format: Article in Journal/Newspaper
Language:English
Published: Nature 2023
Subjects:
Online Access:https://hdl.handle.net/11250/3097799
https://doi.org/10.1038/s41561-023-01273-5
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spelling ftunivbergen:oai:bora.uib.no:11250/3097799 2023-11-12T04:07:53+01:00 Warming beneath an East Antarctic ice shelf due to increased subpolar westerlies and reduced sea ice Lauber, Julius Hattermann, Tore de Steur, Laura Chiche, Elin Maria Kristina Darelius Auger, Matthis Nøst, Ole Anders Moholdt, Geir 2023 application/pdf https://hdl.handle.net/11250/3097799 https://doi.org/10.1038/s41561-023-01273-5 eng eng Nature Norges forskningsråd: 295075 urn:issn:1752-0894 https://hdl.handle.net/11250/3097799 https://doi.org/10.1038/s41561-023-01273-5 cristin:2178627 Nature Geoscience. 2023, 16, 877–885. Navngivelse 4.0 Internasjonal http://creativecommons.org/licenses/by/4.0/deed.no Copyright 2023 The Author(s) Nature Geoscience 877–885 16 Antarktis Antarctica Fysisk oseanografi Physical oceanography Ice ocean interactions VDP::Oseanografi: 452 VDP::Oceanography: 452 Journal article Peer reviewed 2023 ftunivbergen https://doi.org/10.1038/s41561-023-01273-5 2023-10-25T23:08:29Z Understanding how climate change influences ocean-driven melting of the Antarctic ice shelves is one of the greatest challenges for projecting future sea level rise. The East Antarctic ice shelf cavities host cold water masses that limit melting, and only a few short-term observational studies exist on what drives warm water intrusions into these cavities. We analyse nine years of continuous oceanographic records from below Fimbulisen and relate them to oceanic and atmospheric forcing. On monthly time scales, warm inflow events are associated with weakened coastal easterlies reducing downwelling in front of the ice shelf. Since 2016, however, we observe sustained warming, with inflowing Warm Deep Water temperatures reaching above 0 °C. This is concurrent with an increase in satellite-derived basal melt rates of 0.62 m/yr, which nearly doubles the basal mass loss at this relatively cold ice shelf cavity. We find that this transition is linked to a reduction in coastal sea ice cover through an increase in atmosphere–ocean momentum transfer and to a strengthening of remote subpolar westerlies. These results imply that East Antarctic ice shelves may become more exposed to warmer waters with a projected increase of circum-Antarctic westerlies, increasing this region’s relevance for sea level rise projections. publishedVersion Article in Journal/Newspaper Antarc* Antarctic Antarctica Antarktis* Ice Shelf Ice Shelves Sea ice University of Bergen: Bergen Open Research Archive (BORA-UiB) Antarctic The Antarctic Fimbulisen ENVELOPE(-0.500,-0.500,-70.750,-70.750) Nature Geoscience 16 10 877 885
institution Open Polar
collection University of Bergen: Bergen Open Research Archive (BORA-UiB)
op_collection_id ftunivbergen
language English
topic Antarktis
Antarctica
Fysisk oseanografi
Physical oceanography
Ice ocean interactions
VDP::Oseanografi: 452
VDP::Oceanography: 452
spellingShingle Antarktis
Antarctica
Fysisk oseanografi
Physical oceanography
Ice ocean interactions
VDP::Oseanografi: 452
VDP::Oceanography: 452
Lauber, Julius
Hattermann, Tore
de Steur, Laura
Chiche, Elin Maria Kristina Darelius
Auger, Matthis
Nøst, Ole Anders
Moholdt, Geir
Warming beneath an East Antarctic ice shelf due to increased subpolar westerlies and reduced sea ice
topic_facet Antarktis
Antarctica
Fysisk oseanografi
Physical oceanography
Ice ocean interactions
VDP::Oseanografi: 452
VDP::Oceanography: 452
description Understanding how climate change influences ocean-driven melting of the Antarctic ice shelves is one of the greatest challenges for projecting future sea level rise. The East Antarctic ice shelf cavities host cold water masses that limit melting, and only a few short-term observational studies exist on what drives warm water intrusions into these cavities. We analyse nine years of continuous oceanographic records from below Fimbulisen and relate them to oceanic and atmospheric forcing. On monthly time scales, warm inflow events are associated with weakened coastal easterlies reducing downwelling in front of the ice shelf. Since 2016, however, we observe sustained warming, with inflowing Warm Deep Water temperatures reaching above 0 °C. This is concurrent with an increase in satellite-derived basal melt rates of 0.62 m/yr, which nearly doubles the basal mass loss at this relatively cold ice shelf cavity. We find that this transition is linked to a reduction in coastal sea ice cover through an increase in atmosphere–ocean momentum transfer and to a strengthening of remote subpolar westerlies. These results imply that East Antarctic ice shelves may become more exposed to warmer waters with a projected increase of circum-Antarctic westerlies, increasing this region’s relevance for sea level rise projections. publishedVersion
format Article in Journal/Newspaper
author Lauber, Julius
Hattermann, Tore
de Steur, Laura
Chiche, Elin Maria Kristina Darelius
Auger, Matthis
Nøst, Ole Anders
Moholdt, Geir
author_facet Lauber, Julius
Hattermann, Tore
de Steur, Laura
Chiche, Elin Maria Kristina Darelius
Auger, Matthis
Nøst, Ole Anders
Moholdt, Geir
author_sort Lauber, Julius
title Warming beneath an East Antarctic ice shelf due to increased subpolar westerlies and reduced sea ice
title_short Warming beneath an East Antarctic ice shelf due to increased subpolar westerlies and reduced sea ice
title_full Warming beneath an East Antarctic ice shelf due to increased subpolar westerlies and reduced sea ice
title_fullStr Warming beneath an East Antarctic ice shelf due to increased subpolar westerlies and reduced sea ice
title_full_unstemmed Warming beneath an East Antarctic ice shelf due to increased subpolar westerlies and reduced sea ice
title_sort warming beneath an east antarctic ice shelf due to increased subpolar westerlies and reduced sea ice
publisher Nature
publishDate 2023
url https://hdl.handle.net/11250/3097799
https://doi.org/10.1038/s41561-023-01273-5
long_lat ENVELOPE(-0.500,-0.500,-70.750,-70.750)
geographic Antarctic
The Antarctic
Fimbulisen
geographic_facet Antarctic
The Antarctic
Fimbulisen
genre Antarc*
Antarctic
Antarctica
Antarktis*
Ice Shelf
Ice Shelves
Sea ice
genre_facet Antarc*
Antarctic
Antarctica
Antarktis*
Ice Shelf
Ice Shelves
Sea ice
op_source Nature Geoscience
877–885
16
op_relation Norges forskningsråd: 295075
urn:issn:1752-0894
https://hdl.handle.net/11250/3097799
https://doi.org/10.1038/s41561-023-01273-5
cristin:2178627
Nature Geoscience. 2023, 16, 877–885.
op_rights Navngivelse 4.0 Internasjonal
http://creativecommons.org/licenses/by/4.0/deed.no
Copyright 2023 The Author(s)
op_doi https://doi.org/10.1038/s41561-023-01273-5
container_title Nature Geoscience
container_volume 16
container_issue 10
container_start_page 877
op_container_end_page 885
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