Articles | Volume 14, issue 11
https://doi.org/10.5194/cp-14-1755-2018
https://doi.org/10.5194/cp-14-1755-2018
Research article
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20 Nov 2018
Research article | Highlight paper |  | 20 Nov 2018

Connecting the Greenland ice-core and U∕Th timescales via cosmogenic radionuclides: testing the synchroneity of Dansgaard–Oeschger events

Florian Adolphi, Christopher Bronk Ramsey, Tobias Erhardt, R. Lawrence Edwards, Hai Cheng, Chris S. M. Turney, Alan Cooper, Anders Svensson, Sune O. Rasmussen, Hubertus Fischer, and Raimund Muscheler

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Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (05 Oct 2018) by Denis-Didier Rousseau
AR by Florian Adolphi on behalf of the Authors (07 Oct 2018)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (16 Oct 2018) by Denis-Didier Rousseau
RR by Paula Reimer (29 Oct 2018)
RR by Niklas Boers (30 Oct 2018)
ED: Publish subject to technical corrections (31 Oct 2018) by Denis-Didier Rousseau
AR by Florian Adolphi on behalf of the Authors (01 Nov 2018)  Author's response   Manuscript 
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Short summary
The last glacial period was characterized by a number of rapid climate changes seen, for example, as abrupt warmings in Greenland and changes in monsoon rainfall intensity. However, due to chronological uncertainties it is challenging to know how tightly coupled these changes were. Here we exploit cosmogenic signals caused by changes in the Sun and Earth magnetic fields to link different climate archives and improve our understanding of the dynamics of abrupt climate change.