428 ERYUAN LIANG ET AL.Tree growth decline exhibited a regionally synchronous and coherent pattern innorthern China, which is a reflection of drought variability. Based on the studiedtree-ring sites, the 1920s drought extended across North China, southern Ningxia,eastern Qinghai, Gansu and eastern Xinjiang in Northwest China. Dendroclimaticevidence is clearly supported by a variety of historical records. This research alsoshows the need to extend the tree-ring network, to enable a more detailed assessmentof the spatio-temporal characteristics of extreme drought events. Ultimately, thelarge-scale spatio-temporal climate anomalies recovered from an extensive treeringnetwork would provide insights into the atmospheric circulation patterns thatinfluenced precipitation patterns over the semi-arid areas in northern China.AcknowledgementsThis research was supported by the Knowledge Innovation Project of CAS (KZCX3-SW-321) and the National Natural Science Foundation of China (30300053 and90102005). We gratefully acknowledge Professor Raymond S. Bradley for encouragingus to write this paper, and for insightful comments and suggestions on anearlier version of the manuscript. Thanks to Dr. Jürg Luterbacher for many usefulsuggestions and Tom Cannavino for helpful English corrections. We sincerelythank Jingyun Zheng and Hongbin Liu for their suggestions, and Zhaochen Kong,Xudong Chen, Kejun Che, Hu Hao, Tianyu Li, Jicheng He, Lusan Liu and Pu Wufor their help with the fieldwork. The authors also wish to thank to the anonymousreviewers and the editor whose comments and suggestions were helpful inthe improvement of the quality of this paper.ReferencesBradley, R. S. and Jones, P. D.: 1992, Climate Since A.D. 1500, Routledge, London, p. 679.Bryson, R. A. and Swain, A. M.: 1981, ‘Holocene variations of monsoon rainfall in Rajasthan’, Quat.Res. 16, 135–145.Chen, G. R. and Cheng, G. W.: 1997, ‘Drought analysis in the upper basin of changjiang riverand disaster prevention/abatement’, Resources and Environment in the Yangtze Valley 6, 74–79.(in Chinese with English abstract)Chinese Academy of Meteorological Science: 1981, Yearly Charts of Dryness/Wetness in China forthe Last 500-Year Period, China Map Press, Beijing, p. 332. (in Chinese with English abstract)Chu, K. Z., Tu, C. W., and Chang, P. K.: 1936, The Chinese Rainfall, The National Research Instituteof Meteorology, Academic Sinica, Beijing, p. 536. (in Chinese with English abstract)Cook, E. R.: 1992, ‘Using tree rings to study past El Niño/Southern oscillation influences on climate’,in Diaz, H. F. and Markgraf, V. (eds), El Niño: Historical and Paleoclimatic Aspects of the SouthernOscillation, Cambridge University Press, Cambridge, pp. 203–214.Cook, E. R. and Kairiukstis, L.: 1990, Methods of Dendrochronology: Applications in the EnvironmentalSciences, Kluwer Academic Publishers, Dordrecht, pp. 23–217.Cook, E. R., Meko, D. M., Stahle, D. W., and Cleaveland, M. K.: 1999, ‘Drought reconstructions forthe continental united states’, J. Clim. 12, 1145–1162.
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