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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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. 
Bates, G. T.: Influence of the Atlantic multidecadal oscillation on the winter climate of East China, Adv. Atmos. Sci., 24, 126–135, 2007. 
Chen, F., Yuan, Y., Wei, W., Yu, S., and Zhang, T.: Tree ring-based winter temperature reconstruction for Changting, Fujian, subtropical region of Southeast China, since 1850: linkages to the Pacific Ocean, Theor. Appl. Climatol., 109, 141–151, 2012. 
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.