Articles | Volume 16, issue 6
Clim. Past, 16, 2153–2172, 2020
https://doi.org/10.5194/cp-16-2153-2020
Clim. Past, 16, 2153–2172, 2020
https://doi.org/10.5194/cp-16-2153-2020

Research article 11 Nov 2020

Research article | 11 Nov 2020

A 2600-year summer climate reconstruction in central Japan by integrating tree-ring stable oxygen and hydrogen isotopes

Takeshi Nakatsuka 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 May 2020) by Hans Linderholm
AR by Takeshi Nakatsuka on behalf of the Authors (07 Aug 2020)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (16 Aug 2020) by Hans Linderholm
RR by Anonymous Referee #2 (24 Aug 2020)
RR by Anonymous Referee #1 (05 Sep 2020)
ED: Publish subject to technical corrections (21 Sep 2020) by Hans Linderholm
AR by Takeshi Nakatsuka on behalf of the Authors (29 Sep 2020)  Author's response    Manuscript
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Short summary
In general, it is not easy to reconstruct past climate variations over a wide band of frequencies using a single proxy. Here, we propose a new method to reconstruct past summer climate seamlessly from annual to millennial timescales by integrating tree-ring cellulose oxygen and hydrogen isotope ratios. The result can be utilized to investigate various scales of climatological phenomena in the past and climate–society relationships in long human history.