The spatial structure of the 128 ka Antarctic sea ice minimum
We compare multi-ice core data with δ18O model output for the early last interglacial Antarctic sea-ice minimum. The spatial pattern of δ18O across Antarctica is sensitive to the spatial pattern of sea-ice retreat. Local sea ice retreat increases the proportion of winter precipitation, depleting δ18...
Main Authors: | , , , , , , |
---|---|
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Wiley
2017
|
Subjects: | |
Online Access: | https://www.repository.cam.ac.uk/handle/1810/273542 https://doi.org/10.17863/CAM.20616 |
id |
ftunivcam:oai:www.repository.cam.ac.uk:1810/273542 |
---|---|
record_format |
openpolar |
spelling |
ftunivcam:oai:www.repository.cam.ac.uk:1810/273542 2024-02-04T09:55:55+01:00 The spatial structure of the 128 ka Antarctic sea ice minimum Holloway, M Sime, LC Allen, CS Hillenbrand, C-D Bunch, P Wolff, EW Valdes, PJ 2017-11-16 application/pdf https://www.repository.cam.ac.uk/handle/1810/273542 https://doi.org/10.17863/CAM.20616 eng eng Wiley http://dx.doi.org/10.1002/2017gl074594 Geophysical Research Letters https://www.repository.cam.ac.uk/handle/1810/273542 doi:10.17863/CAM.20616 Attribution 4.0 International http://creativecommons.org/licenses/by/4.0/ Antarctic sea ice last interglacial 128 ka ice cores sediment cores Article 2017 ftunivcam https://doi.org/10.17863/CAM.20616 2024-01-11T23:19:27Z We compare multi-ice core data with δ18O model output for the early last interglacial Antarctic sea-ice minimum. The spatial pattern of δ18O across Antarctica is sensitive to the spatial pattern of sea-ice retreat. Local sea ice retreat increases the proportion of winter precipitation, depleting δ18O at ice core sites. However, retreat also enriches δ18O because of the reduced source to-site distance for atmospheric vapour. The joint overall effect is for δ18O to increase as sea ice is reduced. Our data-model comparison indicates a winter sea-ice retreat of 67, 59 and 43 % relative to pre-industrial in the Atlantic, Indian and Pacific sectors of the Southern Ocean. A compilation of Southern Ocean sea-ice proxy data provides weak support for this reconstruction. However, most published marine core sites are located too far north of the 128,000 years BP sea ice edge, preventing independent corroboration for this sea ice reconstruction. This work was funded by NERC grant numbers NE/P009271/1, NE/P013279/1 and NE/K004514/1. MH was also supported by the EPSRC-funded Past Earth Network (Grant number EP/M008363/1). EW is supported by a Royal Society Professorship. Article in Journal/Newspaper Antarc* Antarctic Antarctica ice core Sea ice Southern Ocean Apollo - University of Cambridge Repository Antarctic Southern Ocean Pacific Indian |
institution |
Open Polar |
collection |
Apollo - University of Cambridge Repository |
op_collection_id |
ftunivcam |
language |
English |
topic |
Antarctic sea ice last interglacial 128 ka ice cores sediment cores |
spellingShingle |
Antarctic sea ice last interglacial 128 ka ice cores sediment cores Holloway, M Sime, LC Allen, CS Hillenbrand, C-D Bunch, P Wolff, EW Valdes, PJ The spatial structure of the 128 ka Antarctic sea ice minimum |
topic_facet |
Antarctic sea ice last interglacial 128 ka ice cores sediment cores |
description |
We compare multi-ice core data with δ18O model output for the early last interglacial Antarctic sea-ice minimum. The spatial pattern of δ18O across Antarctica is sensitive to the spatial pattern of sea-ice retreat. Local sea ice retreat increases the proportion of winter precipitation, depleting δ18O at ice core sites. However, retreat also enriches δ18O because of the reduced source to-site distance for atmospheric vapour. The joint overall effect is for δ18O to increase as sea ice is reduced. Our data-model comparison indicates a winter sea-ice retreat of 67, 59 and 43 % relative to pre-industrial in the Atlantic, Indian and Pacific sectors of the Southern Ocean. A compilation of Southern Ocean sea-ice proxy data provides weak support for this reconstruction. However, most published marine core sites are located too far north of the 128,000 years BP sea ice edge, preventing independent corroboration for this sea ice reconstruction. This work was funded by NERC grant numbers NE/P009271/1, NE/P013279/1 and NE/K004514/1. MH was also supported by the EPSRC-funded Past Earth Network (Grant number EP/M008363/1). EW is supported by a Royal Society Professorship. |
format |
Article in Journal/Newspaper |
author |
Holloway, M Sime, LC Allen, CS Hillenbrand, C-D Bunch, P Wolff, EW Valdes, PJ |
author_facet |
Holloway, M Sime, LC Allen, CS Hillenbrand, C-D Bunch, P Wolff, EW Valdes, PJ |
author_sort |
Holloway, M |
title |
The spatial structure of the 128 ka Antarctic sea ice minimum |
title_short |
The spatial structure of the 128 ka Antarctic sea ice minimum |
title_full |
The spatial structure of the 128 ka Antarctic sea ice minimum |
title_fullStr |
The spatial structure of the 128 ka Antarctic sea ice minimum |
title_full_unstemmed |
The spatial structure of the 128 ka Antarctic sea ice minimum |
title_sort |
spatial structure of the 128 ka antarctic sea ice minimum |
publisher |
Wiley |
publishDate |
2017 |
url |
https://www.repository.cam.ac.uk/handle/1810/273542 https://doi.org/10.17863/CAM.20616 |
geographic |
Antarctic Southern Ocean Pacific Indian |
geographic_facet |
Antarctic Southern Ocean Pacific Indian |
genre |
Antarc* Antarctic Antarctica ice core Sea ice Southern Ocean |
genre_facet |
Antarc* Antarctic Antarctica ice core Sea ice Southern Ocean |
op_relation |
https://www.repository.cam.ac.uk/handle/1810/273542 doi:10.17863/CAM.20616 |
op_rights |
Attribution 4.0 International http://creativecommons.org/licenses/by/4.0/ |
op_doi |
https://doi.org/10.17863/CAM.20616 |
_version_ |
1789960134164742144 |