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
刘艺阗1,2(
), 姚济敏1(), 赵林1, 肖瑶1, 乔永平1, 史健宗1
), 姚济敏1(), 赵林1, 肖瑶1, 乔永平1, 史健宗1
Surface energy processes during freeze-thaw cycle in Tanggula permafrost region of Qinghai-Tibet Plateau
Yitian LIU1,2(), Jimin YAO1(), Lin ZHAO1, Yao XIAO1, Yongping QIAO1, Jianzong SHI1
), Jimin YAO1(), Lin ZHAO1, Yao XIAO1, Yongping QIAO1, Jianzong SHI1
图6. 土壤不同状态时地表土壤能量平衡分量日变化
Fig.6. Diurnal variation of surface soil energy fluxes in different soil states
