祁连山俄博岭地区热融洼地与冻胀草丘活动层融化深度差异性对比研究
杜冉1(
), 彭小清1(), 金浩东1, 魏庆1, 孙文1, 贾诗超1, 范成彦1, 王昆1, 魏思浩1, 赵耀华1, FRAUENFELD Oliver W.2
), 彭小清1(), 金浩东1, 魏庆1, 孙文1, 贾诗超1, 范成彦1, 王昆1, 魏思浩1, 赵耀华1, FRAUENFELD Oliver W.2
Comparative study on active layer depth differences between hummocks and thermokarst depressions in the Eboling area of the Qilian Mountains
Ran DU1(), Xiaoqing PENG1(), Haodong JIN1, Qing WEI1, Wen SUN1, Shichao JIA1, Chengyan FAN1, Kun WANG1, Sihao WEI1, Yaohua ZHAO1, Oliver W. FRAUENFELD2
), Xiaoqing PENG1(), Haodong JIN1, Qing WEI1, Wen SUN1, Shichao JIA1, Chengyan FAN1, Kun WANG1, Sihao WEI1, Yaohua ZHAO1, Oliver W. FRAUENFELD2
图1. 祁连山黑河流域俄博岭多年冻土区（a）［
Fig.1. The permafrost regions in Eboling Heihe River Basin in the Qilian Mountains （a）， locations of quadrats （b， c， d）
