中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Tree ring-dated fluctuation history of Midui glacier since the little ice age in the southeastern Tibetan plateau

文献类型:SCI/SSCI论文

作者Xu P. ; Zhu H. F. ; Shao X. M. ; Yin Z. Y.
发表日期2012
关键词Tibetan Plateau glacier fluctuation tree ring Little Ice Age climate change moraine dating north patagonian icefield south asian monsoon late holocene canadian cordillera maritime glaciers mountains alaska himalayan climate dendrochronology
英文摘要Fluctuation history of Midui glacier in the southeastern Tibet since the Little Ice Age (LIA) was reconstructed by the dating of lateral and terminal moraines using tree rings. Four conversions of glacier advance/stabilization to retreat were identified at around 1767, 1875, 1924 and 1964. The glacier reached its LIA maximum position at 1767. The fluctuations are consistent with those of other glaciers from the Tibetan Plateau, the Rockies and the Alps, suggesting high spatial coherency of glacier fluctuations in the Northern Hemisphere. Comparison with the summer temperature reconstruction in the southeastern Tibetan Plateau indicated that the Midui glacier fluctuation may be related to temperature variation on the centennial timescale. On the decadal scale, the fluctuation could correspond to cold/warm variation with an 8-year lag on average.
出处Science China-Earth Sciences
55
4
521-529
收录类别SCI
语种英语
ISSN号1674-7313
源URL[http://ir.igsnrr.ac.cn/handle/311030/26732]  
专题地理科学与资源研究所_历年回溯文献
推荐引用方式
GB/T 7714
Xu P.,Zhu H. F.,Shao X. M.,et al. Tree ring-dated fluctuation history of Midui glacier since the little ice age in the southeastern Tibetan plateau. 2012.

入库方式: OAI收割

来源:地理科学与资源研究所

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