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11. 模拟得到2019—2020年冻胀草丘和热融洼地不同深度的土壤温度差值
Fig.11. Soil temperature difference between the hummocks and thermokarst depressions at different depths in 2019—2020 by modeling
