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《Journal of Glaciology and Geocryology》 2006-04
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Degradation of Permafrost in the Da and Xiao Hinggan Mountains,Northeast China,and Preliminary Assessment of Its Trend

JIN Hui-jun~1, YU Shao-peng~1,2, GUO Dong-xin~1, L Lan-zhi~1, LI Ying-wu~1,3(1.State Key Laboratory of Frozen Soils Engineering,CAREERI,CAS,Lanzhou Gansu 730000,China;2.Department of Geography,Harbin Institute,Harbin Heilongjiang 150001,China; 3.Yitulihe Office,Qiqihar Branch of the Harbin Railway Department,Yakeshi Inner Mongolia 022168,China)  
In the southern margin of permafrost zone of the Eurasian continent,permafrost in the Da and Xiao Hinggan Mountains is warm,thin,thermally unstable and subsequently sensitive to climatic warming.During the past 40 years,permafrost has been degrading as evidenced by deepening active layer,thinning of permafrost,rising ground temperatures,expansion of taliks,and disappearance of permafrost islands.Detailed analyses indicate that climatic warming and sharp reduction of forest coverage during the past century are the general and basic reasons for the degradation of permafrost,and increasing human activities have been accelerating the retreat of permafrost.Based on the close correlations between the southern limit of permafrost(SLP) and decadal average air temperatures,present positions of the SLP are delineated using the multi-year average air temperature isotherms of-1.0~1.0 ℃ during 1999-2000.The SLP would shift northwards upon a projected warming of 1.0~1.5 ℃ during the next 40~50 years,but with significant uneven variations in different parts.
【Fund】: 中国科学院百人计划项目”气候变化条件下温暖多年冻土区线性工程稳定性”(2004407)资助
【CateGory Index】: P642.14
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