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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Bibliografische Detailangaben

Hauptverfasser:	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
Sprache:	Inglês
Veröffentlicht:	MDPI AG 2022-07-01
Schriftenreihe:	Remote Sensing
Schlagworte:	freeze–thaw cycle active layer seasonal deformation SBAS-InSAR Qinghai-Tibet Plateau
Online-Zugang:	https://www.mdpi.com/2072-4292/14/13/3168
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