Articles | Volume 14, issue 11
Clim. Past, 14, 1755–1781, 2018
https://doi.org/10.5194/cp-14-1755-2018
Clim. Past, 14, 1755–1781, 2018
https://doi.org/10.5194/cp-14-1755-2018

Research article 20 Nov 2018

Research article | 20 Nov 2018

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

Florian Adolphi et al.

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Interactive discussion

Status: closed
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.