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首页> 外文期刊>IEEE Geoscience and Remote Sensing Letters >An Improved Two-Step Multitemporal SAR Interferometry Method for Precursory Slope Deformation Detection Over Nanyu Landslide
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An Improved Two-Step Multitemporal SAR Interferometry Method for Precursory Slope Deformation Detection Over Nanyu Landslide

机译:一种改进的两步多型SAR干涉方法,用于南宇滑坡的前兆斜坡变形检测方法

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摘要

A major landslide in Nanyu township, Zhouqu county, Western China, occurred on July 12, 2018, causing widespread damage and blocking the Bailong river. As a widely used surface deformation measurement technique, persistent scatterer interferometry (PSI) method fails in the precursory slope deformation detection over Nanyu landslide for two reasons: the high rate slope deformation of the landslide body before the occurrence of the disaster and the low density of measurement points in the widespread nonurban regions over hillside area. To solve these problems, a two-step multitemporal interferometric synthetic aperture radar (MTInSAR) method is proposed in this letter. In the proposed method, first, a carefully designed small baseline subsets (SBASs) method is applied to extract the linear high rate deformation component, which is then subtracted from the wrapping interferogram to reduce the likelihood of signal aliasing. In the second step, a two-tier network-based MTInSAR method by exploiting both persistent scatterers (PSs) and distributed scatterers (DSs) is employed to retrieve the residual deformation. The proposed method is applied to 47 Sentinel-1 images acquired between December 2016 and July 2018 and successfully detects the precursory deformation over Nanyu landslide for the first time. Experiment results illustrate the advantage of the proposed method for measuring high rate deformation compared with the traditional PSI. By using the proposed algorithm, the deformation rate map shows a clear landslide boundary and precursors of the rapid slope movements with a maximum displacement rate of 483 mm/year along the line of sight of the satellite.
机译:南乌乡,中国西部南峪乡的一个主要滑坡于2018年7月12日发生,造成广泛的损坏并阻挡了百隆河。作为一种广泛使用的表面变形测量技术,持久性散射器干涉测量法(PSI)方法在南宇滑坡上的前兆斜坡变形检测中出现了两个原因:山体内体在灾害发生之前的高速倾斜变形和低密度在山坡区域广泛的非金地区的测量点。为了解决这些问题,在这封信中提出了一种两步多型干涉性合成孔径雷达(MTINSAR)方法。在所提出的方法中,首先,应用精心设计的小基线子集(SBASS)方法来提取线性高速率变形分量,然后从包装干涉图中减去以降低信号混叠的可能性。在第二步中,采用持久性散射器(PSS)和分布式散射器(DSS)来检测残余变形,通过利用两个基于网络的MTINSAR方法来检索残余变形。该方法适用于2016年12月至2018年12月之间获得的47个哨兵-1图像,并在第一次成功地检测南乌山体滑坡的前兆变形。实验结果说明了与传统PSI相比测量高速变形的提出方法的优点。通过使用所提出的算法,变形速率图显示了透明坡度边界和快速坡度运动的前体,其沿着卫星视线的最大位移率为483毫米/年。

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