Last Interglacial subsurface warming on the Antarctic shelf triggered by reduced deep-ocean convection
Abstract The Antarctic ice-sheet could have contributed 3 to 5 m sea-level equivalent to the Last Interglacial sea-level highstand. Such an Antarctic ice-mass loss compared to pre-industrial requires a subsurface warming on the Antarctic shelf of ~ 3 °C according to ice-sheet modelling studies. Here...
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ftdoajarticles:oai:doaj.org/article:f28a62a08a3e451199c6299ed35f36e6 2024-09-15T17:48:15+00:00 Last Interglacial subsurface warming on the Antarctic shelf triggered by reduced deep-ocean convection Nicholas King-Hei Yeung Laurie Menviel Katrin J. Meissner Dipayan Choudhury Tilo Ziehn Matthew A. Chamberlain 2024-04-01T00:00:00Z https://doi.org/10.1038/s43247-024-01383-x https://doaj.org/article/f28a62a08a3e451199c6299ed35f36e6 EN eng Nature Portfolio https://doi.org/10.1038/s43247-024-01383-x https://doaj.org/toc/2662-4435 doi:10.1038/s43247-024-01383-x 2662-4435 https://doaj.org/article/f28a62a08a3e451199c6299ed35f36e6 Communications Earth & Environment, Vol 5, Iss 1, Pp 1-9 (2024) Geology QE1-996.5 Environmental sciences GE1-350 article 2024 ftdoajarticles https://doi.org/10.1038/s43247-024-01383-x 2024-08-05T17:49:33Z Abstract The Antarctic ice-sheet could have contributed 3 to 5 m sea-level equivalent to the Last Interglacial sea-level highstand. Such an Antarctic ice-mass loss compared to pre-industrial requires a subsurface warming on the Antarctic shelf of ~ 3 °C according to ice-sheet modelling studies. Here we show that a substantial subsurface warming is simulated south of 60 °S in an equilibrium experiment of the Last Interglacial. It averages +1.2 °C at ~ 500 m depth from 70 °W to 160 °E, and it reaches +2.4 °C near the Lazarev Sea. Weaker deep-ocean convection due to reduced sea-ice formation is the primary driver of this warming. The associated changes in meridional density gradients and surface winds lead to a weakened Antarctic Circumpolar Current and strengthened Antarctic Slope Current, which further impact subsurface temperatures. A subsurface warming on the Antarctic shelf that could trigger ice-mass loss from the Antarctic ice-sheet can thus be obtained during warm periods from reduced sea-ice formation. Article in Journal/Newspaper Antarc* Antarctic Ice Sheet Lazarev Sea Sea ice Directory of Open Access Journals: DOAJ Articles Communications Earth & Environment 5 1 |
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Open Polar |
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Directory of Open Access Journals: DOAJ Articles |
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ftdoajarticles |
language |
English |
topic |
Geology QE1-996.5 Environmental sciences GE1-350 |
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Geology QE1-996.5 Environmental sciences GE1-350 Nicholas King-Hei Yeung Laurie Menviel Katrin J. Meissner Dipayan Choudhury Tilo Ziehn Matthew A. Chamberlain Last Interglacial subsurface warming on the Antarctic shelf triggered by reduced deep-ocean convection |
topic_facet |
Geology QE1-996.5 Environmental sciences GE1-350 |
description |
Abstract The Antarctic ice-sheet could have contributed 3 to 5 m sea-level equivalent to the Last Interglacial sea-level highstand. Such an Antarctic ice-mass loss compared to pre-industrial requires a subsurface warming on the Antarctic shelf of ~ 3 °C according to ice-sheet modelling studies. Here we show that a substantial subsurface warming is simulated south of 60 °S in an equilibrium experiment of the Last Interglacial. It averages +1.2 °C at ~ 500 m depth from 70 °W to 160 °E, and it reaches +2.4 °C near the Lazarev Sea. Weaker deep-ocean convection due to reduced sea-ice formation is the primary driver of this warming. The associated changes in meridional density gradients and surface winds lead to a weakened Antarctic Circumpolar Current and strengthened Antarctic Slope Current, which further impact subsurface temperatures. A subsurface warming on the Antarctic shelf that could trigger ice-mass loss from the Antarctic ice-sheet can thus be obtained during warm periods from reduced sea-ice formation. |
format |
Article in Journal/Newspaper |
author |
Nicholas King-Hei Yeung Laurie Menviel Katrin J. Meissner Dipayan Choudhury Tilo Ziehn Matthew A. Chamberlain |
author_facet |
Nicholas King-Hei Yeung Laurie Menviel Katrin J. Meissner Dipayan Choudhury Tilo Ziehn Matthew A. Chamberlain |
author_sort |
Nicholas King-Hei Yeung |
title |
Last Interglacial subsurface warming on the Antarctic shelf triggered by reduced deep-ocean convection |
title_short |
Last Interglacial subsurface warming on the Antarctic shelf triggered by reduced deep-ocean convection |
title_full |
Last Interglacial subsurface warming on the Antarctic shelf triggered by reduced deep-ocean convection |
title_fullStr |
Last Interglacial subsurface warming on the Antarctic shelf triggered by reduced deep-ocean convection |
title_full_unstemmed |
Last Interglacial subsurface warming on the Antarctic shelf triggered by reduced deep-ocean convection |
title_sort |
last interglacial subsurface warming on the antarctic shelf triggered by reduced deep-ocean convection |
publisher |
Nature Portfolio |
publishDate |
2024 |
url |
https://doi.org/10.1038/s43247-024-01383-x https://doaj.org/article/f28a62a08a3e451199c6299ed35f36e6 |
genre |
Antarc* Antarctic Ice Sheet Lazarev Sea Sea ice |
genre_facet |
Antarc* Antarctic Ice Sheet Lazarev Sea Sea ice |
op_source |
Communications Earth & Environment, Vol 5, Iss 1, Pp 1-9 (2024) |
op_relation |
https://doi.org/10.1038/s43247-024-01383-x https://doaj.org/toc/2662-4435 doi:10.1038/s43247-024-01383-x 2662-4435 https://doaj.org/article/f28a62a08a3e451199c6299ed35f36e6 |
op_doi |
https://doi.org/10.1038/s43247-024-01383-x |
container_title |
Communications Earth & Environment |
container_volume |
5 |
container_issue |
1 |
_version_ |
1810289415810973696 |