Direct north-south synchronization of abrupt climate change record in ice cores using Beryllium 10

A new, decadally resolved record of the 10Be peak at 41 kyr from the EPICA Dome C ice core (Antarctica) is used to match it with the same peak in the GRIP ice core (Greenland). This permits a direct synchronisation of the climatic variations around this time period, independent of uncertainties rela...

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Bibliographic Details
Published in:Climate of the Past
Main Authors: Raisbeck, G. M., Yiou, F., Jouzel, J., Stocker, T. F.
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2007
Subjects:
article
Verlagsveröffentlichung
Antarctic
Greenland
Antarc*
Antarctica
EPICA
GRIP
ice core
Online Access:https://doi.org/10.5194/cp-3-541-2007
https://noa.gwlb.de/receive/cop_mods_00032158
https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00032112/cp-3-541-2007.pdf
https://cp.copernicus.org/articles/3/541/2007/cp-3-541-2007.pdf
Description
Summary:A new, decadally resolved record of the 10Be peak at 41 kyr from the EPICA Dome C ice core (Antarctica) is used to match it with the same peak in the GRIP ice core (Greenland). This permits a direct synchronisation of the climatic variations around this time period, independent of uncertainties related to the ice age-gas age difference in ice cores. Dansgaard-Oeschger event 10 is in the period of best synchronisation and is found to be coeval with an Antarctic temperature maximum. Simulations using a thermal bipolar seesaw model agree reasonably well with the observed relative climate chronology in these two cores. They also reproduce three Antarctic warming events observed between A1 and A2.

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