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Characterization of the giant landslide at Wenjiagou by the insar technique using TSX-TDX CoSSC data

机译:使用TSX-TDX CoSSC数据的insar技术表征温家沟的巨大滑坡

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摘要

A landslide map is the most basic element for any landslide assessment, especially for giant landslides. However, due to remoteness and hazards, it is difficult to know the characteristics of these landslides after great earthquakes. In this study, the Coregistered Single look Slant range Complex(CoSSC) synthetic aperture radar (SAR) data from TerraSAR-X and its twin satellite TanDEM-X are employed to estimate a high-accuracy digital elevation model (DEM) for the giant landslide in Wenjiagou on Feb. 1, 2013, which was one of the biggest landslides triggered by the 2008 Wenchuan great earthquake. Then, compared to the DEM from SRTM, the elevation change can be estimated, and the characteristics of the Wenjiagou landslide, such as the source and deposit area, are highlighted. Based on the estimation of elevation change, the initial and deposit volumes are estimated as 5.09 x 10(7) m(3) and 4.47 x 10(7) m(3) respectively which are in agreement with previous field investigations by other researchers. And the results also show that using bistatic space-borne SAR data is an effective means for timely assessment of the giant landslide.
机译:滑坡图是任何滑坡评估(尤其是巨型滑坡)中最基本的元素。然而,由于地处偏远和危险,很难知道大地震后这些滑坡的特征。在这项研究中,来自TerraSAR-X及其双卫星TanDEM-X的共注册单视场斜面复杂(CoSSC)合成孔径雷达(SAR)数据被用来估算巨型滑坡的高精度数字高程模型(DEM) 2013年2月1日在温家沟发生的滑坡,是2008年汶川大地震引发的最大滑坡之一。然后,与SRTM的DEM相比,可以估算出高程变化,并突出显示了温家沟滑坡的特征,如源头和沉积区。根据海拔变化的估计,初始和沉积量分别估计为5.09 x 10(7)m(3)和4.47 x 10(7)m(3),这与其他研究人员先前的实地调查一致。结果还表明,利用双基地星载SAR数据是及时评估巨型滑坡的有效手段。

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