Interaction between permafrost and infrastructure along the Qinghai–Tibet Railway detected via jointly analysis of C- and L-band small baseline SAR interferometry

The Qinghai–Tibet Railway (QTR) is the highest and longest plateau linear structure in the world. The embankment is prone to instability, primarily due to the freezing and thawing of the permafrost overlying active layer. The infrastructure construction changes environmental conditions and in turn h...

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Published inRemote sensing of environment Vol. 123; pp. 532 - 540
Main Authors Chen, Fulong, Lin, Hui, Li, Zhen, Chen, Quan, Zhou, Jianmin
Format Journal Article
LanguageEnglish
Published New York, NY Elsevier Inc 01.08.2012
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Abstract The Qinghai–Tibet Railway (QTR) is the highest and longest plateau linear structure in the world. The embankment is prone to instability, primarily due to the freezing and thawing of the permafrost overlying active layer. The infrastructure construction changes environmental conditions and in turn has influenced permafrost evolutions. In this study, we have investigated the feasibility of extracting surface motions in permafrost regions by means of satellite SAR interferometry. The relationship between surface deformation, permafrost active layer and other environmental conditions were further analyzed. In total, 19 L-band ALOS PALSAR SLC images (acquired from 21 June 2007 to 30 December, 2010) and 38 C-band Envisat ASAR SLC images (acquired from 18 November 2004 to 17 December, 2009) were employed to cover the Beiluhe experimental site, Qinghai, China. A hybrid persistent scatterer interferometry model based on interferometric point target analysis (IPTA) and small baseline strategy was firstly developed for surface motion estimation, minimizing the seasonal decorrelation effect. Then, the results from C- and L-band data were analyzed and compared, based on a statistical calibration model. Ground leveling data acquired from Fenghuo Mount Tunnel front with a one month interval were used for InSAR-derived results validation, revealing good agreement in displacement rates as well as time series. The QTR has been in operation since 2006. Our study has observed distinct surface motions along the embankment, primarily in the range of −20 to +20mm/yr, implying the necessity of continued satellite-based surveillance along the QTR. ► We monitor the surface motion along Qinghai–Tibet Railway by C- and L-band InSAR. ► The interaction between permafrost and infrastructure is analyzed. ► A persistent scatterer interferometry model is developed for surface motion inversion. ► The results are further validated by the ground measurements. ► This study implies the necessity for continued monitoring along the QTR.
AbstractList The Qinghai–Tibet Railway (QTR) is the highest and longest plateau linear structure in the world. The embankment is prone to instability, primarily due to the freezing and thawing of the permafrost overlying active layer. The infrastructure construction changes environmental conditions and in turn has influenced permafrost evolutions. In this study, we have investigated the feasibility of extracting surface motions in permafrost regions by means of satellite SAR interferometry. The relationship between surface deformation, permafrost active layer and other environmental conditions were further analyzed. In total, 19 L-band ALOS PALSAR SLC images (acquired from 21 June 2007 to 30 December, 2010) and 38 C-band Envisat ASAR SLC images (acquired from 18 November 2004 to 17 December, 2009) were employed to cover the Beiluhe experimental site, Qinghai, China. A hybrid persistent scatterer interferometry model based on interferometric point target analysis (IPTA) and small baseline strategy was firstly developed for surface motion estimation, minimizing the seasonal decorrelation effect. Then, the results from C- and L-band data were analyzed and compared, based on a statistical calibration model. Ground leveling data acquired from Fenghuo Mount Tunnel front with a one month interval were used for InSAR-derived results validation, revealing good agreement in displacement rates as well as time series. The QTR has been in operation since 2006. Our study has observed distinct surface motions along the embankment, primarily in the range of −20 to +20mm/yr, implying the necessity of continued satellite-based surveillance along the QTR.
The Qinghai–Tibet Railway (QTR) is the highest and longest plateau linear structure in the world. The embankment is prone to instability, primarily due to the freezing and thawing of the permafrost overlying active layer. The infrastructure construction changes environmental conditions and in turn has influenced permafrost evolutions. In this study, we have investigated the feasibility of extracting surface motions in permafrost regions by means of satellite SAR interferometry. The relationship between surface deformation, permafrost active layer and other environmental conditions were further analyzed. In total, 19 L-band ALOS PALSAR SLC images (acquired from 21 June 2007 to 30 December, 2010) and 38 C-band Envisat ASAR SLC images (acquired from 18 November 2004 to 17 December, 2009) were employed to cover the Beiluhe experimental site, Qinghai, China. A hybrid persistent scatterer interferometry model based on interferometric point target analysis (IPTA) and small baseline strategy was firstly developed for surface motion estimation, minimizing the seasonal decorrelation effect. Then, the results from C- and L-band data were analyzed and compared, based on a statistical calibration model. Ground leveling data acquired from Fenghuo Mount Tunnel front with a one month interval were used for InSAR-derived results validation, revealing good agreement in displacement rates as well as time series. The QTR has been in operation since 2006. Our study has observed distinct surface motions along the embankment, primarily in the range of −20 to +20mm/yr, implying the necessity of continued satellite-based surveillance along the QTR. ► We monitor the surface motion along Qinghai–Tibet Railway by C- and L-band InSAR. ► The interaction between permafrost and infrastructure is analyzed. ► A persistent scatterer interferometry model is developed for surface motion inversion. ► The results are further validated by the ground measurements. ► This study implies the necessity for continued monitoring along the QTR.
Author Li, Zhen
Chen, Quan
Zhou, Jianmin
Chen, Fulong
Lin, Hui
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  surname: Zhou
  fullname: Zhou, Jianmin
  organization: Center for Earth Observation and Digital Earth, Chinese Academy of Sciences, No.9 Dengzhuang South Road, Haidian District, Beijing 100094, China
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Keywords Surface motion
Permafrost
Qinghai–Tibet Railway
Small baseline
SAR interferometry
Railway
embankments
Environmental factor
Thawing
global
Image
Relation
Qinghai-Tibet Railway
plateaus
soils
Structure
Synthetic aperture radar
detection
Small
Interaction
interferometry
L band
evolution
baseline
analysis
freezing
permafrost
instability
Surface deformation
Feasibility
infrastructures
movement
Language English
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SSID ssj0015871
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Snippet The Qinghai–Tibet Railway (QTR) is the highest and longest plateau linear structure in the world. The embankment is prone to instability, primarily due to the...
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SubjectTerms Animal, plant and microbial ecology
Applied geophysics
Biological and medical sciences
China
deformation
Earth sciences
Earth, ocean, space
environmental factors
Exact sciences and technology
freezing
Fundamental and applied biological sciences. Psychology
General aspects. Techniques
infrastructure
interferometry
Internal geophysics
monitoring
Permafrost
plateaus
Qinghai–Tibet Railway
remote sensing
SAR interferometry
satellites
Small baseline
Surface motion
Teledetection and vegetation maps
thawing
time series analysis
Title Interaction between permafrost and infrastructure along the Qinghai–Tibet Railway detected via jointly analysis of C- and L-band small baseline SAR interferometry
URI https://dx.doi.org/10.1016/j.rse.2012.04.020
https://www.proquest.com/docview/1710234432
Volume 123
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