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Climate of the Past An interactive open-access journal of the European Geosciences Union
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Volume 12, issue 7
Clim. Past, 12, 1485–1498, 2016
https://doi.org/10.5194/cp-12-1485-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
Clim. Past, 12, 1485–1498, 2016
https://doi.org/10.5194/cp-12-1485-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 13 Jul 2016

Research article | 13 Jul 2016

A 368-year maximum temperature reconstruction based on tree-ring data in the northwestern Sichuan Plateau (NWSP), China

Liangjun Zhu et al.

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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 (13 Apr 2016) by Eduardo Zorita
AR by Xiaochun Wang on behalf of the Authors (15 Apr 2016)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (18 Apr 2016) by Eduardo Zorita
RR by Anonymous Referee #2 (13 Jun 2016)
ED: Publish as is (16 Jun 2016) by Eduardo Zorita
Publications Copernicus
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Short summary
We present a 368-year late summer maximum temperature reconstruction based on spruce tree rings. It touches on the critical topic of climate reconstruction in the eastern edge of Tibetan Plateau and represents an extension and enhancement of climate records for this area. The Little Ice Age was well represented and 20th century warming was not obvious in this reconstruction. This temperature variation may be affected by global land–sea atmospheric circulation as well as solar and volcanic forcing.
We present a 368-year late summer maximum temperature reconstruction based on spruce tree rings....
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