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REMOTE SENSING FOR LAND & RESOURCES    2008, Vol. 20 Issue (3) : 15-19     DOI: 10.6046/gtzyyg.2008.03.04
Technology and Methodology |
A STUDY OF DEFORMATION IN PERMAFROST REGIONS OF QINGHAI-TIBET PLATEAU BASED ON ALOS/PALSAR D-InSAR INTERFEROMETRY
XIE Chou1,2, LI Zhen2,3, LI Xin-wu2,3
1. Graduate School of Chinese Academy of Sciences, Beijing 100039, China; 2. State Key Laboratory of Remote Sensing Science,Jointly Sponsored by Institute of Remote Sensing Applications of Chinese Academy of Sciences and Beijing Normal University,Beijing 100101, China; 3. Center for Earth Observation and Digital Earth, Chinese Academy of Sciences, Beijing 100039, China
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Abstract  

 Surface displacement resulting from seasonal freezing bulge and thawing subsidence constitutes a main

hazard to engineering construction of permafrost regions, especially to the Qinghai-Tibet railway. One of the main

problems that the Qinghai-Tibet railway encounters is the effective detection of the displacement field. The

interferometric SAR technique has the capability for measuring ground deformation in a wide range of application.

PALSAR can keep high coherence in interferometry over non-urban areas, thus very suitable for analyzing

deformation over permafrost regions of Qinghai-Tibet Plateau. This paper presents the method of PALSAR

interferometry for analyzing ground surface displacement. The proposed technique was implemented by using ENVISAT

ASAR images to detect the deformation over permafrost regions of Qinghai-Tibet Plateau, and the results are in

accordance with the results obtained by a traditional ground leveling method. Such an achievement encourages

future utilization of PALSAR interferometry to analyze deformation of the frozen earth in Qinghai-Tibet Plateau.

Keywords Suspended silt      Spectra reflectivity      Remote sensing monitoring     
Issue Date: 06 July 2009
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Zhang Chungui. A STUDY OF DEFORMATION IN PERMAFROST REGIONS OF QINGHAI-TIBET PLATEAU BASED ON ALOS/PALSAR D-InSAR INTERFEROMETRY[J]. REMOTE SENSING FOR LAND & RESOURCES, 2008, 20(3): 15-19.
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https://www.gtzyyg.com/EN/10.6046/gtzyyg.2008.03.04     OR     https://www.gtzyyg.com/EN/Y2008/V20/I3/15
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