青藏高原唐古拉地区活动层厚度分布特征及其影响因素
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杜二计 1,2( ), 杨斌 3, 谭昌海 3, 肖瑶 1, 刘广岳 1,2, 邹德富 1, 赵拥华 1, 吴晓东 1, 吴通华 1, 赵林 4( ), 胡国杰 1, 周华云 1,2, 李智斌 4, 汪易 3
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Distribution characteristics and its influencing factors of active layer thickness in Tanggula area on the Qinghai-Tibet Plateau
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Erji DU 1,2( ), Bin YANG 3, Changhai TAN 3, Yao XIAO 1, Guangyue LIU 1,2, Defu ZOU 1, Yonghua ZHAO 1, Xiaodong WU 1, Tonghua WU 1, Lin ZHAO 4( ), Guojie HU 1, Huayun ZHOU 1,2, Zhibin LI 4, Yi WANG 3
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图4. 活动层厚度变化速率与土壤含水率(θ)、热导率(λ)及地表融化指数(F)的关系
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Fig. 4. Relationship between changing rate of active layer thickness and soil moisture (θ) (a), thermal conductivity (λ) (b) and surface thawing index (F) (c)
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