The relationship between air temperature fluctuation and Glacial Lake Outburst Floods in Tibet, China
文献类型:期刊论文
作者 | Liu, Jing-Jing1,2,3,4,5![]() ![]() ![]() |
刊名 | QUATERNARY INTERNATIONAL
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出版日期 | 2014-02-13 |
卷号 | 321页码:78-87 |
关键词 | Science & Technology |
ISSN号 | 1040-6182 |
通讯作者 | Su, Peng-Cheng |
英文摘要 | In recent years, disasters caused by Glacial Lake Outburst Floods (GLOFs) have taken place more frequently in Tibet than previously and have been the cause of considerable losses. Temperature fluctuations are believed a major influencing factor of GLOFs. However, if or how much climatic change influences GLOFs is a question that remains to be answered. In this paper, using 24 GLOFs related to 19 glacial lakes and temperature data from 14 meteorological stations, we explored the relationships between temperature variations on different temporal scales (annual, monthly, and daily) and GLOFs. There were three active periods for GLOFs in the 1960s, 1980s and 2000s in Tibet, when 16 of 24 GLOFs took place. All the studied GLOFs occurred in the ablation months (from May and September, and especially in July and August) and on ablation days with a monthly average temperature and daily average temperature that were both greater than 0 degrees C. Based on the analysis of monthly and daily temperature, GLOFs depend on the coupled influence of ablation temperature and accumulation temperature; even the accumulation temperature may be important. Based on this, temperature increments were defined, representing the change from accumulation to ablation temperature with a significant impact on GLOFs. There is an altitude effect on GLOFs, in that lakes at lower altitude generally burst earlier, whereas those at a higher altitude burst later. The monthly and daily increments increase according to a similar power-law form with elevation. (C) 2013 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] | CLIMATE-CHANGE ; SPATIAL INTERPOLATION ; LATE PLEISTOCENE ; DAMMED LAKES ; HIMALAYA ; PLATEAU ; REGION ; CORE ; ASIA ; CONSEQUENCES |
收录类别 | SCI |
语种 | 英语 |
WOS记录号 | WOS:000331853500012 |
源URL | [http://ir.imde.ac.cn/handle/131551/9939] ![]() |
专题 | 成都山地灾害与环境研究所_山地灾害与地表过程重点实验室 |
作者单位 | 1.Chinese Acad Sci, Inst Mt Hazards & Environm, Chengdu 610041, Peoples R China 2.Chinese Acad Sci, Key Lab Mt Hazards & Surface Proc, Chengdu 610041, Peoples R China 3.Minist Water Conservancy & Power, Chengdu 610041, Peoples R China 4.China Inst Water Resources & Hydropower Res, State Key Lab Simulat & Regulat Water Cycle River, Beijing 100038, Peoples R China 5.Chinese Acad Sci, Grad Univ, Beijing 100039, Peoples R China |
推荐引用方式 GB/T 7714 | Liu, Jing-Jing,Cheng, Zun-Lan,Su, Peng-Cheng. The relationship between air temperature fluctuation and Glacial Lake Outburst Floods in Tibet, China[J]. QUATERNARY INTERNATIONAL,2014,321:78-87. |
APA | Liu, Jing-Jing,Cheng, Zun-Lan,&Su, Peng-Cheng.(2014).The relationship between air temperature fluctuation and Glacial Lake Outburst Floods in Tibet, China.QUATERNARY INTERNATIONAL,321,78-87. |
MLA | Liu, Jing-Jing,et al."The relationship between air temperature fluctuation and Glacial Lake Outburst Floods in Tibet, China".QUATERNARY INTERNATIONAL 321(2014):78-87. |
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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