Time‐series InSAR monitoring of surface deformation in Yakutsk, a city located on continuous permafrost

Мониторинг поверхностных деформаций методом временных рядов InSAR в Якутске, городе, расположенном на непрерывном вечномерзлом слое
M. N. Zheleznyak, Hao Wei, Xianglong Li, Ze Zhang, Huijun Jin, Shengrong Zhang, Jinbang Zhai, Andrey Melnikov, Leonid Gagarin
2023-11-02

Persistent Scatterer Interferometric Synthetic Aperture RadarSentinel-1BTime-series InSARYakutsk surface deformationpermafrost thaw subsidence
Abstract Permafrost, known for its high sensitivity to climate change and human activities, plays a crucial role in comprehending the environmental sustainability of Arctic cities. Yakutsk, being the largest city situated in continuous permafrost, has suffered irreversible damage to surface buildings due to the widespread permafrost thaw. Therefore, it is imperative to conduct detailed monitoring and assessment of surface deformation to ensure the stable operation of building facilities and to plan urban development situated above the permafrost. This study utilized 138 scenes of Sentinel‐1B images captured between 2017 and 2021 to process the surface deformation variations of Yakutsk using the Persistent Scatterer Interferometric Synthetic Aperture Radar (PS‐InSAR) method. The surface deformation rate map reflects that the study area is undergoing extensive surface subsidence. The cumulative deformation time series maps effectively trace the temporal and spatial evolution of surface deformation, with the highest surface subsidence rates exceeding 40 mm/year and maximum cumulative subsidence exceeding 250 mm. In‐depth analysis of the obtained results indicated that the permafrost in Yakutsk is undergoing degradation, and the primary reason for surface subsidence is the thawing of foundation soils and the degradation of ice‐bearing permafrost. This study provides basic data for the investigation of geohazards caused by surface subsidence in Yakutsk.
1
Analysis indicates permafrost degradation is occurring in Yakutsk, with thawing foundation soils and degradation of ice‑bearing permafrost as primary causes.
2
Cumulative deformation time series effectively trace temporal and spatial evolution of subsidence between 2017 and 2021.
3
Observed maximum subsidence rates exceed 40 mm/year and maximum cumulative subsidence exceeds 250 mm.
4
The results provide baseline data for assessing geohazards and planning stable urban development on permafrost in Yakutsk.
5
The surface deformation rate map shows extensive surface subsidence across the study area.
6
Using 138 Sentinel‑1B scenes (2017–2021) and PS‑InSAR, the study mapped surface deformation in Yakutsk on continuous permafrost.

Surface of Yakutsk city (ground and foundation soils on continuous permafrost) monitored by time-series InSAR

Temporal and spatial surface deformation (subsidence) rates and cumulative displacement caused by permafrost thaw and degradation of ice-bearing foundation soils, as retrieved by PS‑InSAR from Sentinel‑1B (2017–2021)

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2023-11-02
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M. N. Zheleznyak
Hao Wei
Xianglong Li
Ze Zhang
Huijun Jin
Shengrong Zhang
Jinbang Zhai
Andrey Melnikov
Leonid Gagarin
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