The spatial structure of the 128 ka Antarctic sea ice minimum
Geophysical Research Letters
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Holloway, M., Sime, L., Allen, C., Hillenbrand, C., Bunch, P., Wolff, E., & Valdes, P. (2017). The spatial structure of the 128 ka Antarctic sea ice minimum. Geophysical Research Letters, 44 (21), 129-139. https://doi.org/10.1002/2017GL074594
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.
Antarctic, sea ice, last interglacial, 128 ka, ice cores, sediment cores
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.
Royal Society (RP120096)
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External DOI: https://doi.org/10.1002/2017GL074594
This record's URL: https://www.repository.cam.ac.uk/handle/1810/273542
Attribution 4.0 International
Licence URL: http://creativecommons.org/licenses/by/4.0/
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