Articles | Volume 16, issue 1
https://doi.org/10.5194/cp-16-29-2020
https://doi.org/10.5194/cp-16-29-2020
Research article
 | 
08 Jan 2020
Research article |  | 08 Jan 2020

NALPS19: sub-orbital-scale climate variability recorded in northern Alpine speleothems during the last glacial period

Gina E. Moseley, Christoph Spötl, Susanne Brandstätter, Tobias Erhardt, Marc Luetscher, and R. Lawrence Edwards

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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 (31 Jul 2019) by Dominik Fleitmann
AR by Anna Mirena Feist-Polner on behalf of the Authors (13 Sep 2019)  Author's response
ED: Referee Nomination & Report Request started (02 Oct 2019) by Dominik Fleitmann
RR by Anonymous Referee #2 (03 Oct 2019)
RR by Anonymous Referee #1 (25 Oct 2019)
ED: Publish subject to technical corrections (18 Nov 2019) by Dominik Fleitmann
AR by Gina E. Moseley on behalf of the Authors (21 Nov 2019)  Author's response    Manuscript

Post-review adjustments

AA: Author's adjustment | EA: Editor approval
AA by Gina E. Moseley on behalf of the Authors (19 Dec 2019)   Author's adjustment  
EA: Adjustments approved (06 Jan 2020) by Dominik Fleitmann
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Short summary
Abrupt climate change during the last ice age can be used to provide important insights into the timescales on which the climate is capable of changing and the mechanisms that drive those changes. In this study, we construct climate records for the period 60 to 120 ka using stalagmites that formed in caves along the northern rim of the European Alps and find good agreement with the timing of climate changes in Greenland and the Asian monsoon.