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
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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
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Comparative study on active layer depth differences between hummocks and thermokarst depressions in the Eboling area of the Qilian Mountains
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Ran DU 1( ), Xiaoqing PENG 1( ), Haodong JIN 1, Qing WEI 1, Wen SUN 1, Shichao JIA 1, Chengyan FAN 1, Kun WANG 1, Sihao WEI 1, Yaohua ZHAO 1, Oliver W. FRAUENFELD 2
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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
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Fig.11. Soil temperature difference between the hummocks and thermokarst depressions at different depths in 2019—2020 by modeling
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