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《Journal of Beijing Forestry University》 2006-S2
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Climatic response of tree-ring width from alpine treeline in the middle of Anyemaqen Mountains, northeastern Tibetan Plateau,China

PENG Jian-feng~1;GOU Xiao-hua~1;CHEN Fa-hu~1;LIU Pu-xing~ 1,2 ;ZHANG Yong~1;FANG Ke-yan~1. 1 Center for Arid Environment and Paleoclimate Research(CAEP),Key Laboratory of Western China's Environment System, Ministry of Education, Lanzhou University, 730000, P.R. China; 2 College of Geography and Environment Sciences, Northwest Normal University, Lanzhou,730070, P.R. China.  
Based on the cores of Juniperus przewalskii from alpine treeline in the middle Anymaqin Mountains, northeastern Tibetan Plateau, the authors developed the tree-ring width index standard chronologies. The results showed that characteristics of chronology had more climatic information, and tree-ring width was significant and positively correlated with the mean temperature in July. There was remarkable consistency between tree-ring width curve and July mean temperature in weather data recorded during 1959-2001. However, It was found that there was preferably consistency between tree-ring width curve and July mean temperature during 1976-2001. The results indicted that low temperature and excessive rain in July were main limited factors. The results of cycle analysis showed that the main periods were century and two permit-oscillations in 193 years. Tree-growth in alpine treeline held a high-temperature and arid period, which was general period during 1920-1930's in northwestern China, and the authors also found that it was the coldest and longest period during 1861-1878 in last 200 years.
【Fund】: 国家自然科学基金创新群体基金项目(40421101);; 国家自然科学基金重点项目(40671191、90502008)
【CateGory Index】: S716.3
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