Article ; Online: East Antarctic warming forced by ice loss during the Last Interglacial.
2024 Volume 15, Issue 1, Page(s) 1026
Abstract: ... surface warming over East Antarctica of 2 to 4 °C, and sea surface temperature (SST) increases ... in the Weddell and Ross Seas by up to 2 °C. Meltwater forcing causes a high latitude SST decrease and ... a subsurface (100-500 m) ocean temperature increase by up to 2 °C in the Ross Sea. Our results suggest ...
Abstract | During the Last Interglacial (LIG; 129-116 thousand years before present), the Antarctic ice sheet (AIS) was 1 to 7 m sea level equivalent smaller than at pre-industrial. Here, we assess the climatic impact of partial AIS melting at the LIG by forcing a coupled climate model with a smaller AIS and the equivalent meltwater input around the Antarctic coast. We find that changes in surface elevation induce surface warming over East Antarctica of 2 to 4 °C, and sea surface temperature (SST) increases in the Weddell and Ross Seas by up to 2 °C. Meltwater forcing causes a high latitude SST decrease and a subsurface (100-500 m) ocean temperature increase by up to 2 °C in the Ross Sea. Our results suggest that the combination of a smaller AIS and enhanced meltwater input leads to a larger sub-surface warming than meltwater alone and induces further Antarctic warming than each perturbation separately. |
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Language | English |
Publishing date | 2024-02-03 |
Publishing country | England |
Document type | Journal Article |
ZDB-ID | 2553671-0 |
ISSN | 2041-1723 ; 2041-1723 |
ISSN (online) | 2041-1723 |
ISSN | 2041-1723 |
DOI | 10.1038/s41467-024-45501-x |
Database | MEDical Literature Analysis and Retrieval System OnLINE |
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