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Characteristics of Freeze–Thaw Cycles in an Endorheic Basin on the Qinghai-Tibet Plateau Based on SBAS-InSAR Technology

The freeze–thaw (F-T) cycle of the active layer (AL) causes the “frost heave and thaw settlement” deformation of the terrain surface. Accurately identifying its amplitude and time characteristics is important for climate, hydrology, and ecology research in permafrost regions. We used Sentinel-1 SAR...

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Principais autores: Huayun Zhou, Lin Zhao, Lingxiao Wang, Zanpin Xing, Defu Zou, Guojie Hu, Changwei Xie, Qiangqiang Pang, Guangyue Liu, Erji Du, Shibo Liu, Yongping Qiao, Jianting Zhao, Zhibin Li, Yadong Liu
Format: Artigo
Sprog:Inglês
Udgivet: MDPI AG 2022-07-01
Serier:Remote Sensing
Fag:
freeze–thaw cycle
active layer
seasonal deformation
SBAS-InSAR
Qinghai-Tibet Plateau
Online adgang:https://www.mdpi.com/2072-4292/14/13/3168
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