Revealing the impacts of environmental and anthropogenic factors on permafrost deformation in the central Qinghai-Tibet Plateau using InSAR and interpretable machine learning

• Interpretable ML reveals environmental impacts on permafrost deformation. • Soil hydrothermal effects are nonlinear, with moisture as the key driver. • Long-term vegetation changes regulate deformation in permafrost regions. • Differentiated impacts of infrastructure and human activities on deformation. Permafrost stability on the Qinghai-Tibet Plateau (QTP) is vital amid environmental changes and human activities. Interferometric Synthetic Aperture Radar (InSAR) effectively monitors permafrost deformation, capturing seasonal and long-term trends via active layer hydrothermal shifts. While prior studies emphasized large-scale deformation, finer-scale regulatory effects of environmental factors and human activities remain underexplored. We used Small Baseline Subset (SBAS)-InSAR to derive ground deformation time series and developed an XGBoost-based model to assess impacts of soil hydrothermal conditions, vegetation, terrain, and human activities. Our results show that soil moisture plays a dominant role in permafrost deformation, with its interaction with soil temperature exhibiting nonlinear effects on permafrost deformation. Long-term changes in Normalized Difference Vegetation Index (NDVI) were significantly positively correlated with the seasonal deformation amplitude (R 2 = 0.3546, p < 0.001). Geomorphons exerted significant control, with valleys and lowlands exhibiting reduced permafrost deformation due to distinct hydrothermal conditions, whereas highlands demonstrated greater stability. Human infrastructure further influenced ground deformation. The Wudaoliang (WDL) Train Station (median subsidence rate: −11.55 mm/yr) and Qinghai-Tibet Railway (median subsidence rate: −8.75 mm/yr) exhibited strong regulatory effects, whereas WDL Town (median subsidence rate: −12.45 mm/yr) and the Qinghai-Tibet Highway (median subsidence rate: −10.32 mm/yr) experienced more pronounced deformation, which highlights the importance of engineering design in mitigating permafrost degradation. The results provide new insights into the regulatory mechanisms of environmental factors and human activities on permafrost deformation across the QTP using interpretable machine learning (ML), which is important for environmental conservation and engineering disaster prevention in permafrost regions.

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Publication Details

Journal
Ecological Indicators
Published
2025-08-05
DOI
https://doi.org/10.1016/j.ecolind.2025.113977
Citations
1
Primary Topic
Climate change and permafrost
Type
article
Field-Weighted Citation Impact
1.30

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article

Revealing the impacts of environmental and anthropogenic factors on permafrost deformation in the central Qinghai-Tibet Plateau using InSAR and interpretable machine learning

Jianjun Chen, Tonghua Wu, Peiqing Lou, Jie Chen et al.
1 citations
Ecological Indicators
Climate change and permafrost
1.30
article

Revealing the impacts of environmental and anthropogenic factors on permafrost deformation in the central Qinghai-Tibet Plateau using InSAR and interpretable machine learning

Jianjun Chen, Tonghua Wu, Peiqing Lou, Jie Chen, Xiaofan Zhu, Ren Li, Xingchen Lin
article en
1 citations

Abstract

• Interpretable ML reveals environmental impacts on permafrost deformation. • Soil hydrothermal effects are nonlinear, with moisture as the key driver. • Long-term vegetation changes regulate deformation in permafrost regions. • Differentiated impacts of infrastructure and human activities on deformation. Permafrost stability on the Qinghai-Tibet Plateau (QTP) is vital amid environmental changes and human activities. Interferometric Synthetic Aperture Radar (InSAR) effectively monitors permafrost deformation, capturing seasonal and long-term trends via active layer hydrothermal shifts. While prior studies emphasized large-scale deformation, finer-scale regulatory effects of environmental factors and human activities remain underexplored. We used Small Baseline Subset (SBAS)-InSAR to derive ground deformation time series and developed an XGBoost-based model to assess impacts of soil hydrothermal conditions, vegetation, terrain, and human activities. Our results show that soil moisture plays a dominant role in permafrost deformation, with its interaction with soil temperature exhibiting nonlinear effects on permafrost deformation. Long-term changes in Normalized Difference Vegetation Index (NDVI) were significantly positively correlated with the seasonal deformation amplitude (R 2 = 0.3546, p < 0.001). Geomorphons exerted significant control, with valleys and lowlands exhibiting reduced permafrost deformation due to distinct hydrothermal conditions, whereas highlands demonstrated greater stability. Human infrastructure further influenced ground deformation. The Wudaoliang (WDL) Train Station (median subsidence rate: −11.55 mm/yr) and Qinghai-Tibet Railway (median subsidence rate: −8.75 mm/yr) exhibited strong regulatory effects, whereas WDL Town (median subsidence rate: −12.45 mm/yr) and the Qinghai-Tibet Highway (median subsidence rate: −10.32 mm/yr) experienced more pronounced deformation, which highlights the importance of engineering design in mitigating permafrost degradation. The results provide new insights into the regulatory mechanisms of environmental factors and human activities on permafrost deformation across the QTP using interpretable machine learning (ML), which is important for environmental conservation and engineering disaster prevention in permafrost regions.

Ecological IndicatorsVol. 178
Chinese Academy of Sciences (CN), Guilin University of Technology (CN), Northwest Institute of Eco-Environment and Resources (CN), University of Chinese Academy of Sciences (CN)
Chinese Academy of Sciences, Science and Technology Department of Gansu Province, West Light Foundation of the Chinese Academy of Sciences, State Key Laboratory of Cryospheric Science, Science and Technology Program of Gansu Province
Openalex Percentile: Top 20%
Climate change and permafrost
1.30
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