Articles | Volume 18, issue 7
Clim. Past, 18, 1625–1654, 2022
https://doi.org/10.5194/cp-18-1625-2022
Clim. Past, 18, 1625–1654, 2022
https://doi.org/10.5194/cp-18-1625-2022
Research article
13 Jul 2022
Research article | 13 Jul 2022

Investigating stable oxygen and carbon isotopic variability in speleothem records over the last millennium using multiple isotope-enabled climate models

Janica C. Bühler et al.

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Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on cp-2021-152', Anonymous Referee #1, 29 Dec 2021
    • AC1: 'Reply on RC1', Janica Buehler, 31 Jan 2022
  • RC2: 'Comment on cp-2021-152', Anonymous Referee #2, 04 Feb 2022
    • AC2: 'Reply on RC2', Janica Buehler, 24 Feb 2022

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (09 Mar 2022) by Qiuzhen Yin
AR by Janica Buehler on behalf of the Authors (19 Apr 2022)  Author's response    Author's tracked changes    Manuscript
ED: Referee Nomination & Report Request started (02 May 2022) by Qiuzhen Yin
RR by Anonymous Referee #1 (11 May 2022)
RR by Anonymous Referee #2 (14 May 2022)
ED: Publish subject to minor revisions (review by editor) (15 May 2022) by Qiuzhen Yin
AR by Janica Buehler on behalf of the Authors (03 Jun 2022)  Author's response    Author's tracked changes    Manuscript
ED: Publish as is (06 Jun 2022) by Qiuzhen Yin
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Short summary
We collected and standardized the output of five isotope-enabled simulations for the last millennium and assess differences and similarities to records from a global speleothem database. Modeled isotope variations mostly arise from temperature differences. While lower-resolution speleothems do not capture extreme changes to the extent of models, they show higher variability on multi-decadal timescales. As no model excels in all comparisons, we advise a multi-model approach where possible.