Changes of the Hailuogou glacier, Mt. Gongga, China, against the background of climate change during the Holocene
文献类型:期刊论文
作者 | Li, Zongxing1; He, Yuanqing1,4; Yang, Xiaomei3; Theakstone, Wilfred H.5; Jia, Wenxiong1,3; Pu, Tao4; Liu, Qiao2![]() |
刊名 | QUATERNARY INTERNATIONAL
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出版日期 | 2010-05-01 |
卷号 | 218期号:1-2页码:166-175 |
关键词 | LATE QUATERNARY GLACIATION HIMALAYAN GLACIATION YULONG MOUNTAIN TIBETAN PLATEAU MONSOON SENSITIVITY SIGNALS RETREAT RECORDS REGION |
ISSN号 | 1040-6182 |
通讯作者 | Li, ZX |
英文摘要 | Large changes have occurred at Hailuogou glacier, Mt. Gongga, China, during the Holocene. Various data indicate that it retreated by >1.88 km during the 20th century, and mass balance records show that it suffered a sustained mass loss of snow and ice in the period 1959/60-2003/04, with an accumulated mass balance of -10.83 m water equivalent. Hydrological data demonstrate that runoff from the glacier has been increasing both seasonally and annually, the principal cause being an increase of ice and snow melt water. As the mean temperature in the Hailuogou basin rose by 0.1 degrees C between 1994 and 2004, the runoff increased by 2.6 m(3) s(-1). Changes of glacier morphology which occurred during this period include a decrease of thickness, enlargement of glacial caves, and reduction of the size of seracs. The Hailuogou glacier advanced three times during the Little Ice Age in response to three cold periods in the Mt. Hengduan region. There also were three noticeable advances in the Neoglacial. There was a very clear relationship between glacier change, climate change and forest line change in the period 3000 a BP-100 a BP. Overall, it is clear that changes of the Hailuogou glacier in the Holocene have been responded to climatic fluctuations, but quantitative evaluation of the relationship is difficult owing to the sparse spatial coverage of reliable evidence and the limited available longer term data. (C) 2008 Elsevier Ltd and INQUA. All rights reserved. |
WOS标题词 | Science & Technology ; Physical Sciences |
类目[WOS] | Geography, Physical ; Geosciences, Multidisciplinary |
研究领域[WOS] | Physical Geography ; Geology |
关键词[WOS] | LATE QUATERNARY GLACIATION ; HIMALAYAN GLACIATION ; YULONG MOUNTAIN ; TIBETAN PLATEAU ; MONSOON ; SENSITIVITY ; SIGNALS ; RETREAT ; RECORDS ; REGION |
收录类别 | SCI |
语种 | 英语 |
WOS记录号 | WOS:000278283100017 |
公开日期 | 2013-07-05 |
源URL | [http://ir.imde.ac.cn/handle/131551/5600] ![]() |
专题 | 成都山地灾害与环境研究所_山地表生过程与生态调控重点实验室 |
作者单位 | 1.Chinese Acad Sci, Cold & Arid Reg Environm & Engn Res Inst, State Key Lab Cryosphere Sci, Lijiang Stn, Lanzhou 730000, Peoples R China 2.Chinese Acad Sci, Chengdu Inst Mt Hazards & Environm, Chengdu 610041, Peoples R China 3.NW Normal Univ, Coll Geog & Environm Sci, Lanzhou 730070, Peoples R China 4.Lanzhou Univ, Coll Resources & Environm Sci, Lanzhou 730000, Peoples R China 5.Univ Manchester, Sch Environm & Dev, Manchester M13 9PL, Lancs, England |
推荐引用方式 GB/T 7714 | Li, Zongxing,He, Yuanqing,Yang, Xiaomei,et al. Changes of the Hailuogou glacier, Mt. Gongga, China, against the background of climate change during the Holocene[J]. QUATERNARY INTERNATIONAL,2010,218(1-2):166-175. |
APA | Li, Zongxing.,He, Yuanqing.,Yang, Xiaomei.,Theakstone, Wilfred H..,Jia, Wenxiong.,...&Du, Jiankuo.(2010).Changes of the Hailuogou glacier, Mt. Gongga, China, against the background of climate change during the Holocene.QUATERNARY INTERNATIONAL,218(1-2),166-175. |
MLA | Li, Zongxing,et al."Changes of the Hailuogou glacier, Mt. Gongga, China, against the background of climate change during the Holocene".QUATERNARY INTERNATIONAL 218.1-2(2010):166-175. |
入库方式: OAI收割
来源:成都山地灾害与环境研究所
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