Climate variability features of the last interglacial in the East Antarctic EPICA Dome C ice core

Whereas millennial to sub-millennial climate variability has been identified during the current interglacial period, past interglacial variability features remain poorly explored because of lacking data at sufficient temporal resolutions. Here, we present new deuterium data from the EPICA Dome C ice...

Full description

Bibliographic Details
Published in:Geophysical Research Letters
Main Authors: Pol, K., Masson-Delmotte, V., Cattani, O., Debret, M., Falourd, S., Jouzel, J., Landais, A., Minster, B., Mudelsee, M., Schulz, M., Stenni, B.
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2014
Subjects:
Antarctic
Antarc*
EPICA
ice core
Online Access:http://nora.nerc.ac.uk/id/eprint/507188/
https://nora.nerc.ac.uk/id/eprint/507188/1/grl51679.pdf
https://doi.org/10.1002/2014GL059561
Description
Summary:Whereas millennial to sub-millennial climate variability has been identified during the current interglacial period, past interglacial variability features remain poorly explored because of lacking data at sufficient temporal resolutions. Here, we present new deuterium data from the EPICA Dome C ice core, documenting at decadal resolution temperature changes occurring over the East Antarctic plateau during the warmer-than-today last interglacial. Expanding previous evidence of instabilities during the last interglacial, multi-centennial sub-events are identified and labelled for the first time in a past interglacial context. A variance analysis further reveals two major climatic features. First, an increase in variability is detected prior to the glacial inception, as already observed at the end of Marine Isotopic Stage 11 in the same core. Second, the overall variance level is systematically higher during the last interglacial than during the current one, suggesting that a warmer East Antarctic climate may also be more variable.

Similar Items