天山烏魯木齊河源1號(hào)冰川消融對(duì)氣候變化的響應(yīng)

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   作者單位： 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： 氣候變化研究進(jìn)展  ISTIC 英文刊名： ADVANCES IN CLIMATE CHANGE RESEARCH  年，卷(期)： 2008 4(z1)  分類(lèi)號(hào)： P4  關(guān)鍵詞： glacier melting   climate warming   Tianshan   (U)rümqi Glacier No.1  

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