Articles | Volume 17, issue 3
Clim. Past, 17, 1005–1023, 2021
https://doi.org/10.5194/cp-17-1005-2021
Clim. Past, 17, 1005–1023, 2021
https://doi.org/10.5194/cp-17-1005-2021

Research article 07 May 2021

Research article | 07 May 2021

Large-scale climate signals of a European oxygen isotope network from tree rings

Daniel F. Balting 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 (12 Oct 2020) by Julie Loisel
AR by Daniel Balting on behalf of the Authors (04 Dec 2020)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (22 Dec 2020) by Julie Loisel
RR by Anonymous Referee #2 (26 Jan 2021)
RR by Anonymous Referee #3 (18 Feb 2021)
ED: Publish subject to minor revisions (review by editor) (05 Mar 2021) by Julie Loisel
AR by Daniel Balting on behalf of the Authors (18 Mar 2021)  Author's response    Author's tracked changes    Manuscript
ED: Publish as is (23 Mar 2021) by Julie Loisel
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Short summary
To extend climate information back in time, we investigate the climate sensitivity of a δ18O network from tree rings, consisting of 26 European sites and covering the last 400 years. Our results suggest that the δ18O variability is associated with large-scale anomaly patterns that resemble those observed for the El Niño–Southern Oscillation. We conclude that the investigation of large-scale climate signals far beyond instrumental records can be done with a δ18O network derived from tree rings.