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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:小型基线子集干涉合成孔径雷达和标准偏差椭圆在北京市地面沉降的时空特征

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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1970年代以来,北京发生了地面沉降。形成了五个主要的沉降区域:东郊巴里庄—大角亭,董北郊—莱光英,昌平沙河—巴仙庄,大兴裕发—L县和顺义-平格庄。在这项研究中,我们调查了沉降比较严重的朝阳,顺义和通州地区,并使用2004年至2010年获得的47张ASAR图像和小型基线子集干涉式合成孔径雷达(SBAS InSAR)的数据获得了地面沉降监测结果。 )。在此基础上,我们计算了持久散射点和特征椭圆的空间分布中心,以分析研究区域沉降的时空特征。

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