InSAR技术在多年冻土区形变监测的应用
刘世博1,3(
), 赵林2(), 汪凌霄2, 邹德富1, 周华云1,3, 谢昌卫1, 乔永平1, 岳广阳1, 史健宗1
), 赵林2(), 汪凌霄2, 邹德富1, 周华云1,3, 谢昌卫1, 乔永平1, 岳广阳1, 史健宗1
Application of InSAR technology to monitor deformation in permafrost areas
Shibo LIU1,3(), Lin ZHAO2(), Lingxiao WANG2, Defu ZOU1, Huayun ZHOU1,3, Changwei XIE1, Yongping QIAO1, Guangyang YUE1, Jianzong SHI1
), Lin ZHAO2(), Lingxiao WANG2, Defu ZOU1, Huayun ZHOU1,3, Changwei XIE1, Yongping QIAO1, Guangyang YUE1, Jianzong SHI1
图1. 活动层季节冻融过程
Fig.1. Seasonal freeze-thaw process of active layer
