Articles | Volume 14, issue 8
Clim. Past, 14, 1213–1228, 2018
https://doi.org/10.5194/cp-14-1213-2018
Clim. Past, 14, 1213–1228, 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 et al.

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Cited articles

Bao, G., Liu, Y., Liu, N., and Linderholm, H. W.: Drought variability in eastern Mongolian Plateau and its linkages to the large-scale climate forcing, Clim. Dynam., 44, 717–733, 2015. 
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Chen, F., Yuan, Y., Wei, W., Yu, S., Zhang, T., Shang, H., Zhang, R., Qin, L., and Fan, Z.: Tree-ring recorded hydroclimatic change in Tienshan mountains during the past 500 years, Quaternary Int., 358, 35–41, 2015. 
Cook, E. R. and Kairiukstis, L. A.: Methods of dendrochronology: applications in the environmental sciences, Kluwer Academic Publishers, Dordrecht, 394 pp., 1990. 
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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.