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Climate of the Past An interactive open-access journal of the European Geosciences Union
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CP | Articles | Volume 14, issue 8
Clim. Past, 14, 1213–1228, 2018
https://doi.org/10.5194/cp-14-1213-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
Clim. Past, 14, 1213–1228, 2018
https://doi.org/10.5194/cp-14-1213-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

Research article 15 Aug 2018

Research article | 15 Aug 2018

Response of Pinus sylvestris var. mongolica to water change and drought history reconstruction in the past 260 years, northeast 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 (28 Jun 2018) by Nathalie Combourieu Nebout
AR by Liangjun Zhu on behalf of the Authors (05 Jul 2018)  Author's response    Manuscript
ED: Reconsider after major revisions (09 Jul 2018) by Nathalie Combourieu Nebout
AR by Liangjun Zhu on behalf of the Authors (09 Jul 2018)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (10 Jul 2018) by Nathalie Combourieu Nebout
RR by Anonymous Referee #1 (19 Jul 2018)
RR by Anonymous Referee #2 (20 Jul 2018)
ED: Publish as is (01 Aug 2018) by Nathalie Combourieu Nebout
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Short summary
This paper presents a 260-year tree-ring-based PDSI reconstruction for the central Daxing'an Mountains, northeast China. A warm–wet pattern was identified for the Daxing'an Mountains in recent decades, while a warm–dry pattern was found for the Mongolian Plateau. Overall, the dry/wet variability of the Daxing'an Mountains and its relationship with the surrounding areas might be driven by Pacific and Atlantic Ocean oscillations.
This paper presents a 260-year tree-ring-based PDSI reconstruction for the central Daxing'an...
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