Articles | Volume 14, issue 8
https://doi.org/10.5194/cp-14-1213-2018
https://doi.org/10.5194/cp-14-1213-2018
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, Qichao Yao, David J. Cooper, Shijie Han, and Xiaochun Wang

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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 (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
AR by Liangjun Zhu on behalf of the Authors (03 Aug 2018)
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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.