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Spatiotemporal characteristics of land subsidence in Beijing from small baseline subset interferometric synthetic aperture radar and standard deviational ellipse

机译:小基线北京地区土地沉降的时空特征来自小基线子集干涉合成孔径雷达和标准偏差椭圆

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Land subsidence in Beijing has occurred since the 1970s. Five major subsidence areas have formed: Dongjiao Ba Lizhuang-Da Jiaoting, Dong Beijiao-Lai Guangying, Changping Shahe-Ba Xianzhuang, Daxing Yufa-Lixian, and Shunyi-Ping Gezhuang. In this study, we investigated Chaoyang, Shunyi, and Tongzhou districts, which have experienced relatively serious subsidence, and obtained land subsidence monitoring results using data from 47 ASAR images obtained between 2004 and 2010 and the small baseline subset interferometric synthetic aperture radar (SBAS InSAR). On this basis, we calculated the spatial distribution center of persistent scatterer points and the eigenellipse to analyze the spatiotemporal characteristics of subsidence in the study area.
机译:自20世纪70年代以来,北京的土地沉降已经发生。五大沉降地区已形成:东郊李泉 - 大景,董蓓滨赖广英,昌平沙河 - 巴泉,大兴玉福丽县,顺义坪地庄。在这项研究中,我们调查了朝阳,顺义和通州区,经历了相对严重的沉降,并使用来自2004年至2010年和2010年之间获得的47个ASAR图像的数据以及小基线子集干涉合成孔径雷达(SBAS INSAR)获得了土地沉降监测结果)。在此基础上,我们计算了持久散射点的空间分配中心和特征胶层,分析了研究区沉降的时空特征。

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