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PS-InSAR Monitoring of Landslide Activity in the Black Sea Coast of the Caucasus

机译:PS-InSAR监测高加索黑海沿岸滑坡活动

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摘要

The landslide activity in the area of Bolshoy Sochi (Big Sochi) situated at the Black Sea coast of the Great Caucasus has been studied using the StaMPS PS-InSAR method. We incorporated three sets of radar images from the satellites with different wavelengths ALOS, Envisat and Terra-SAR-X from both ascending and descending tracks which cover the time period from January 2007 to September 2012. Comparative investigation of surface displacements obtained from all the data sets is presented. Areas where high surface displacement rates have been located on the base of the satellite data coincide well with zones of high landslide activity according to ground observations. We constructed time series for the two landslides: in the Baranovka and Mamaika villages where considerable surface movements had been observed during the time of acquisitions. Analysis of the time series made it possible to determine periods of activity and relative stability of the landslides and compare them with ground observations.
机译:使用StaMPS PS-InSAR方法研究了位于大高加索黑海沿岸的大索契(Bolshoy Sochi)地区的滑坡活动。我们从上升和下降轨道合并了三组来自不同波长的卫星ALOS,Envisat和Terra-SAR-X的雷达图像,覆盖了从2007年1月到2012年9月的时间段。从所有数据中获得的地表位移的比较研究套被提出。根据地面观测,在卫星数据的基础上高地表位移率的区域与高滑坡活动区非常吻合。我们为两个滑坡建立了时间序列:在巴拉诺夫卡(Baranovka)村和马马卡(Mamaika)村,在采集期间观察到大量的地面运动。通过对时间序列进行分析,可以确定滑坡的活动周期和相对稳定性,并将其与地面观测结果进行比较。

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