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天山乌鲁木齐河源1号冰川消融对气候变化的响应
Current glacier recession under the global warming has aroused world-wide attention.Initiated from 1958,the observations show that over the past 50 years,the glacier has changed remarkably in the aspects of snow-firn stratigraphy,ice formation zone,ice temperature,area and terminus position,etc.These changes are apparently the results of temperature rise in this area.The glacier recession continued throughout the entire observed time period,and showed an accelerated tendency since 1985.Meltwater runoff also increased 84.2% over the last 20 years.
作 者： 李忠勤 沈永平 Li Huilin Dong Zhiwen Wang Liwei Li Zhongqin Shen Yongping Li Huilin Dong Zhiwen Wang Liwei 作者单位： State Key Laboratory of Cryospheric Science/Tianshan Glaciological Station,Cold and Arid Regions Environmental and Engineering Research Institute,Chinese Academy of Sciences,Lanzhou 730000,China 刊 名： 气候变化研究进展 ISTIC 英文刊名： ADVANCES IN CLIMATE CHANGE RESEARCH 年，卷(期)： 2008 4(z1) 分类号： P4 关键词： glacier melting climate warming Tianshan (U)rümqi Glacier No.1【天山乌鲁木齐河源1号冰川消融对气候变化的响应】相关文章：
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