中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Little Ice Age glacier fluctuations reconstructed for the southeastern Tibetan Plateau using tree rings

文献类型:SCI/SSCI论文

作者Zhu, Haifeng1; Xu, Peng2; Shao, Xuemei2; Luo, Haijiang3
发表日期2013-01-14
英文摘要Long-term records are essential for evaluating recent glacier fluctuation and its linkage to climate change. Moraines of two glaciers (Gawalong glacier and Xincuo glacier) in the southeastern Tibetan Plateau were dated. Germination date of the oldest tree yields a minimum age before 1760s for the outermost lateral moraine of Gawalong glacier in southern Bomi. A tilted tree indicated that the glacier readvanced to its maximum position since the early 20th century at around 1987-1992. Xincuo glacier in eastern Gongbujiangda reached its Little Ice Age (LIA) maximum before 1876. The difference implies that detailed dating of moraines is necessary for studying LIA glacier response to climate change in the study area. Trees growing on LIA glacier deposits proved to be very useful for deriving age estimates of historic glacier fluctuations in the southeastern Tibetan Plateau. (C) 2012 Elsevier Ltd and INQUA. All rights reserved.
出处QUATERNARY INTERNATIONAL
283
134-138
语种英语
源URL[http://192.168.22.105/handle/311030/29983]  
专题地理科学与资源研究所_历年回溯文献
通讯作者Xu, Peng
作者单位1.Chinese Acad Sci, Inst Tibetan Plateau Res, Key Lab Tibetan Environm Changes & Land Surface P, Beijing 100085, Peoples R China
2.Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Beijing 100101, Peoples R China
3.Environm Monitoring Ctr China, Beijing 100012, Peoples R China
推荐引用方式
GB/T 7714
Zhu, Haifeng,Xu, Peng,Shao, Xuemei,et al. Little Ice Age glacier fluctuations reconstructed for the southeastern Tibetan Plateau using tree rings. 2013.

入库方式: OAI收割

来源:地理科学与资源研究所

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