中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Glacial fluctuations around the Karola Pass, eastern Lhagoi Kangri Range, since the Last Glacial Maximum

文献类型:期刊论文

作者Liu, JH (Liu, Jinhua)2,3; Yi, CL (Yi, Chaolu)2,4; Li, YK (Li, Yingkui)1; Bi, WL (Bi, Weili)2,3; Zhang, Q (Zhang, Qian)2,3; Hu, G (Hu, Gang)2; Li, YK
刊名JOURNAL OF QUATERNARY SCIENCE
出版日期2017
卷号32期号:4页码:516-527
关键词COSMOGENIC NUCLIDE CONSTRAINTS LATE QUATERNARY GLACIATION BE-10 SURFACE EXPOSURE TIAN-SHAN PRODUCTION-RATES TIBETAN PLATEAU SURROUNDING MOUNTAINS HOLOCENE MONSOON CLIMATE
DOI10.1002/jqs.2946
文献子类Article
英文摘要Mountain glaciers are sensitive to climate change, especially in climatic transition zones. We investigated Late Quaternary glacial history in two valleys around the Karola Pass of the eastern Lhagoi Kangri Range, central Himalaya, using cosmogenic Be-10 surface exposure dating. Four glacial events were dated to 0.36 +/- 0.09 to 0.13 +/- 0.02 ka (LIA=Little Ice Age), 2.5 +/- 0.2 ka (Neoglacial), 9.7 +/- 0.4 to 8.2 +/- 0.4 ka (Early Holocene) and 23.1 +/- 0.9 to 16.3 +/- 0.7 ka (LGM-LG, LGM=Last Glacial Maximum; LG=Lateglacial). The extent of glacier coverage has reduced successively since the LGM-LG, when ice coverage was about 2.69 times larger than at present (approximate to 2010 CE). Equilibrium line altitude (ELA) values dropped 360, 265, 195 and 120m during the LGM-LG, Early Holocene, Neoglacial and LIA, respectively, compared to the present value. These glacial events were broadly synchronous with other areas in the central Himalaya. It is likely that climate cooling was the major driver of glacial fluctuations during the LGM-LG. Abrupt and short-lived cooling phases, as well as increased Indian monsoonal precipitation, resulted in glacial expansions or standstills during the Early Holocene. In addition, cold and wet climatic conditions were attributed to the Neoglacial and LIA glacial events in this area.
学科主题自然地理学
WOS研究方向Physical Geography; Geology
语种英语
WOS记录号WOS:000401172500006
源URL[http://ir.itpcas.ac.cn/handle/131C11/8250]  
专题青藏高原研究所_图书馆
通讯作者Li, YK
作者单位1.Univ Tennessee, Dept Geog, Knoxville, TN 37996 USA.
2.Chinese Acad Sci, Inst Tibetan Plateau Res, Key Lab Tibetan Environm Changes & Land Surface P, Beijing 100101, Peoples R China.
3.Univ Chinese Acad Sci, Beijing 100049, Peoples R China.
4.Chinese Acad Sci, CAS Ctr Excellence Tibetan Plateau Earth Syst Sci, Beijing 100101, Peoples R China.
推荐引用方式
GB/T 7714
Liu, JH ,Yi, CL ,Li, YK ,et al. Glacial fluctuations around the Karola Pass, eastern Lhagoi Kangri Range, since the Last Glacial Maximum[J]. JOURNAL OF QUATERNARY SCIENCE,2017,32(4):516-527.
APA Liu, JH .,Yi, CL .,Li, YK .,Bi, WL .,Zhang, Q .,...&Li, YK.(2017).Glacial fluctuations around the Karola Pass, eastern Lhagoi Kangri Range, since the Last Glacial Maximum.JOURNAL OF QUATERNARY SCIENCE,32(4),516-527.
MLA Liu, JH ,et al."Glacial fluctuations around the Karola Pass, eastern Lhagoi Kangri Range, since the Last Glacial Maximum".JOURNAL OF QUATERNARY SCIENCE 32.4(2017):516-527.

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来源:青藏高原研究所

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