Mid-Holocene Antarctic sea-ice increase driven by marine ice sheet retreat
Over recent decades Antarctic sea-ice extent has increased, alongside widespread ice shelf thinning and freshening of waters along the Antarctic margin. In contrast, Earth system models generally simulate a decrease in sea ice. Circulation of water masses beneath large-cavity ice shelves is not incl...
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Online Access: | https://oskar-bordeaux.fr/handle/20.500.12278/188612 https://hdl.handle.net/20.500.12278/188612 https://doi.org/10.5194/cp-17-1-2021 |
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ftoskarbordeaux:oai:oskar-bordeaux.fr:20.500.12278/188612 2024-04-07T07:47:15+00:00 Mid-Holocene Antarctic sea-ice increase driven by marine ice sheet retreat ASHLEY, Kate MCKAY, Robert ETOURNEAU, Johan JIMENEZ-ESPEJO, Francisco CONDRON, Alan ALBOT, Anna CROSTA, Xavier RIESSELMAN, Christina SEKI, Osamu MASSÉ, Guillaume GOLLEDGE, Nicholas GASSON, Edward LOWRY, Daniel BARRAND, Nicholas JOHNSON, Katelyn BERTLER, Nancy ESCUTIA, Carlota DUNBAR, Robert BENDLE, James 2021-01-05 https://oskar-bordeaux.fr/handle/20.500.12278/188612 https://hdl.handle.net/20.500.12278/188612 https://doi.org/10.5194/cp-17-1-2021 EN eng 1814-9324 https://oskar-bordeaux.fr/handle/20.500.12278/188612 doi:10.5194/cp-17-1-2021 Attribution 3.0 United States open http://creativecommons.org/licenses/by/3.0/us/ CC BY Planète et Univers [physics]/Sciences de la Terre/Climatologie Planète et Univers [physics]/Sciences de la Terre/Océanographie Planète et Univers [physics]/Océan Atmosphère Article de revue 2021 ftoskarbordeaux https://doi.org/20.500.12278/18861210.5194/cp-17-1-2021 2024-03-14T20:15:21Z Over recent decades Antarctic sea-ice extent has increased, alongside widespread ice shelf thinning and freshening of waters along the Antarctic margin. In contrast, Earth system models generally simulate a decrease in sea ice. Circulation of water masses beneath large-cavity ice shelves is not included in current Earth System models and may be a driver of this phenomena. We examine a Holocene sediment core off East Antarctica that records the Neoglacial transition, the last major baseline shift of Antarctic sea ice, and part of a late-Holocene global cooling trend. We provide a multiproxy record of Holocene glacial meltwater input, sediment transport, and sea-ice variability. Our record, supported by high-resolution ocean modelling, shows that a rapid Antarctic sea-ice increase during the mid-Holocene (∼ 4.5 ka) occurred against a backdrop of increasing glacial meltwater input and gradual climate warming. We suggest that mid-Holocene ice shelf cavity expansion led to cooling of surface waters and sea-ice growth that slowed basal ice shelf melting. Incorporating this feedback mechanism into global climate models will be important for future projections of Antarctic changes. Article in Journal/Newspaper Antarc* Antarctic Antarctica East Antarctica Ice Sheet Ice Shelf Ice Shelves Sea ice OSKAR Bordeaux (Open Science Knowledge ARchive) Antarctic The Antarctic East Antarctica Climate of the Past 17 1 1 19 |
institution |
Open Polar |
collection |
OSKAR Bordeaux (Open Science Knowledge ARchive) |
op_collection_id |
ftoskarbordeaux |
language |
English |
topic |
Planète et Univers [physics]/Sciences de la Terre/Climatologie Planète et Univers [physics]/Sciences de la Terre/Océanographie Planète et Univers [physics]/Océan Atmosphère |
spellingShingle |
Planète et Univers [physics]/Sciences de la Terre/Climatologie Planète et Univers [physics]/Sciences de la Terre/Océanographie Planète et Univers [physics]/Océan Atmosphère ASHLEY, Kate MCKAY, Robert ETOURNEAU, Johan JIMENEZ-ESPEJO, Francisco CONDRON, Alan ALBOT, Anna CROSTA, Xavier RIESSELMAN, Christina SEKI, Osamu MASSÉ, Guillaume GOLLEDGE, Nicholas GASSON, Edward LOWRY, Daniel BARRAND, Nicholas JOHNSON, Katelyn BERTLER, Nancy ESCUTIA, Carlota DUNBAR, Robert BENDLE, James Mid-Holocene Antarctic sea-ice increase driven by marine ice sheet retreat |
topic_facet |
Planète et Univers [physics]/Sciences de la Terre/Climatologie Planète et Univers [physics]/Sciences de la Terre/Océanographie Planète et Univers [physics]/Océan Atmosphère |
description |
Over recent decades Antarctic sea-ice extent has increased, alongside widespread ice shelf thinning and freshening of waters along the Antarctic margin. In contrast, Earth system models generally simulate a decrease in sea ice. Circulation of water masses beneath large-cavity ice shelves is not included in current Earth System models and may be a driver of this phenomena. We examine a Holocene sediment core off East Antarctica that records the Neoglacial transition, the last major baseline shift of Antarctic sea ice, and part of a late-Holocene global cooling trend. We provide a multiproxy record of Holocene glacial meltwater input, sediment transport, and sea-ice variability. Our record, supported by high-resolution ocean modelling, shows that a rapid Antarctic sea-ice increase during the mid-Holocene (∼ 4.5 ka) occurred against a backdrop of increasing glacial meltwater input and gradual climate warming. We suggest that mid-Holocene ice shelf cavity expansion led to cooling of surface waters and sea-ice growth that slowed basal ice shelf melting. Incorporating this feedback mechanism into global climate models will be important for future projections of Antarctic changes. |
format |
Article in Journal/Newspaper |
author |
ASHLEY, Kate MCKAY, Robert ETOURNEAU, Johan JIMENEZ-ESPEJO, Francisco CONDRON, Alan ALBOT, Anna CROSTA, Xavier RIESSELMAN, Christina SEKI, Osamu MASSÉ, Guillaume GOLLEDGE, Nicholas GASSON, Edward LOWRY, Daniel BARRAND, Nicholas JOHNSON, Katelyn BERTLER, Nancy ESCUTIA, Carlota DUNBAR, Robert BENDLE, James |
author_facet |
ASHLEY, Kate MCKAY, Robert ETOURNEAU, Johan JIMENEZ-ESPEJO, Francisco CONDRON, Alan ALBOT, Anna CROSTA, Xavier RIESSELMAN, Christina SEKI, Osamu MASSÉ, Guillaume GOLLEDGE, Nicholas GASSON, Edward LOWRY, Daniel BARRAND, Nicholas JOHNSON, Katelyn BERTLER, Nancy ESCUTIA, Carlota DUNBAR, Robert BENDLE, James |
author_sort |
ASHLEY, Kate |
title |
Mid-Holocene Antarctic sea-ice increase driven by marine ice sheet retreat |
title_short |
Mid-Holocene Antarctic sea-ice increase driven by marine ice sheet retreat |
title_full |
Mid-Holocene Antarctic sea-ice increase driven by marine ice sheet retreat |
title_fullStr |
Mid-Holocene Antarctic sea-ice increase driven by marine ice sheet retreat |
title_full_unstemmed |
Mid-Holocene Antarctic sea-ice increase driven by marine ice sheet retreat |
title_sort |
mid-holocene antarctic sea-ice increase driven by marine ice sheet retreat |
publishDate |
2021 |
url |
https://oskar-bordeaux.fr/handle/20.500.12278/188612 https://hdl.handle.net/20.500.12278/188612 https://doi.org/10.5194/cp-17-1-2021 |
geographic |
Antarctic The Antarctic East Antarctica |
geographic_facet |
Antarctic The Antarctic East Antarctica |
genre |
Antarc* Antarctic Antarctica East Antarctica Ice Sheet Ice Shelf Ice Shelves Sea ice |
genre_facet |
Antarc* Antarctic Antarctica East Antarctica Ice Sheet Ice Shelf Ice Shelves Sea ice |
op_relation |
1814-9324 https://oskar-bordeaux.fr/handle/20.500.12278/188612 doi:10.5194/cp-17-1-2021 |
op_rights |
Attribution 3.0 United States open http://creativecommons.org/licenses/by/3.0/us/ CC BY |
op_doi |
https://doi.org/20.500.12278/18861210.5194/cp-17-1-2021 |
container_title |
Climate of the Past |
container_volume |
17 |
container_issue |
1 |
container_start_page |
1 |
op_container_end_page |
19 |
_version_ |
1795673156841635840 |