青藏高原唐古拉多年冻土区冻融循环过程中的能量平衡特征
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刘艺阗 1,2( ), 姚济敏 1( ), 赵林 1, 肖瑶 1, 乔永平 1, 史健宗 1
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Surface energy processes during freeze-thaw cycle in Tanggula permafrost region of Qinghai-Tibet Plateau
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Yitian LIU 1,2( ), Jimin YAO 1( ), Lin ZHAO 1, Yao XIAO 1, Yongping QIAO 1, Jianzong SHI 1
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图5. 唐古拉站2014年反照率及积雪深度变化值
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Fig.5. Changes in albedo and snow depth of Tanggula in 2014
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