Glacial environments on the Tibetan Plateau and global cooling
文献类型:期刊论文
作者 | Liu, TS; Zhang, XS; Xiong, SF; Qin, XG; Yang, XP |
刊名 | QUATERNARY INTERNATIONAL
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出版日期 | 2002 |
卷号 | 97-8页码:133-139 |
ISSN号 | 1040-6182 |
文献子类 | Article |
英文摘要 | The glacial environments on the Tibetan Plateau and the mechanisms for glacier and snow accumulation are discussed on the basis of new evidence of global temperature fluctuations and regional biome type changes. The biome types show that extensive snow and glacier fields could develop on the Tibetan Plateau with a temperature lowering of 7-9degreesC and precipitation decrease by 30-70%. Considering the cooling effect due to an increase of albedo resulting from increased snow and ice coverage, it is possible that the valley glaciers became enlarged to form large glaciers and snow fields during the Last Glacial Maximum. This new environmental modeling shows that the environmental conditions changed considerably during past glaciations. Such changes might have notable impacts on the monsoons and possibly on global climate. (C) 2002 Published by Elsevier Science Ltd. |
WOS关键词 | SEA-SURFACE TEMPERATURE ; CLIMATE-CHANGE ; ICE CORE ; RECORDS ; MAXIMUM ; WATER ; STAGE |
WOS研究方向 | Physical Geography ; Geology |
语种 | 英语 |
WOS记录号 | WOS:000178859500012 |
出版者 | PERGAMON-ELSEVIER SCIENCE LTD |
源URL | [http://ir.iggcas.ac.cn/handle/132A11/77472] ![]() |
专题 | 中国科学院地质与地球物理研究所 |
通讯作者 | Liu, TS |
作者单位 | 1.Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China 2.Chinese Acad Sci, Inst Bot, Beijing, Peoples R China |
推荐引用方式 GB/T 7714 | Liu, TS,Zhang, XS,Xiong, SF,et al. Glacial environments on the Tibetan Plateau and global cooling[J]. QUATERNARY INTERNATIONAL,2002,97-8:133-139. |
APA | Liu, TS,Zhang, XS,Xiong, SF,Qin, XG,&Yang, XP.(2002).Glacial environments on the Tibetan Plateau and global cooling.QUATERNARY INTERNATIONAL,97-8,133-139. |
MLA | Liu, TS,et al."Glacial environments on the Tibetan Plateau and global cooling".QUATERNARY INTERNATIONAL 97-8(2002):133-139. |
入库方式: OAI收割
来源:地质与地球物理研究所
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