Articles | Volume 17, issue 4
https://doi.org/10.5194/cp-17-1751-2021
https://doi.org/10.5194/cp-17-1751-2021
Research article
 | 
26 Aug 2021
Research article |  | 26 Aug 2021

Significance of uncertain phasing between the onsets of stadial–interstadial transitions in different Greenland ice core proxies

Keno Riechers and Niklas Boers

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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 (04 Feb 2021) by Laurie Menviel
AR by Keno Riechers on behalf of the Authors (15 Apr 2021)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (16 Apr 2021) by Laurie Menviel
RR by Anonymous Referee #1 (11 May 2021)
RR by Anonymous Referee #2 (19 May 2021)
ED: Reconsider after major revisions (20 May 2021) by Laurie Menviel
AR by Keno Riechers on behalf of the Authors (01 Jul 2021)  Author's response    Author's tracked changes    Manuscript
ED: Publish subject to technical corrections (05 Jul 2021) by Laurie Menviel
AR by Keno Riechers on behalf of the Authors (15 Jul 2021)  Author's response    Manuscript

Post-review adjustments

AA: Author's adjustment | EA: Editor approval
AA by Keno Riechers on behalf of the Authors (25 Aug 2021)   Author's adjustment   Manuscript
EA: Adjustments approved (25 Aug 2021) by Laurie Menviel
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Short summary
Greenland ice core data show that the last glacial cycle was punctuated by a series of abrupt climate shifts comprising significant warming over Greenland, retreat of North Atlantic sea ice, and atmospheric reorganization. Statistical analysis of multi-proxy records reveals no systematic lead or lag between the transitions of proxies that represent different climatic subsystems, and hence no evidence for a potential trigger of these so-called Dansgaard–Oeschger events can be found.