姚佳明, 姚鑫, 刘星洪, 陈剑, 李凌婧, 周振凯. 2018: 滑坡D-InSAR观测中的大气误差去除研究以金沙江巧家段为例. 工程地质学报, 26(s1): 14-21. DOI: 10.13544/j.cnki.jeg.2018040
    引用本文: 姚佳明, 姚鑫, 刘星洪, 陈剑, 李凌婧, 周振凯. 2018: 滑坡D-InSAR观测中的大气误差去除研究以金沙江巧家段为例. 工程地质学报, 26(s1): 14-21. DOI: 10.13544/j.cnki.jeg.2018040
    YAO Jiaming, YAO Xin, LIU Xinghong, CHEN Jian, LI Lingjing, ZHOU Zhenkai. 2018: STUDY ON THE ATMOSPHERIC CORRECTION OF D-INSAR REMOVAL BY THREE-DIMENSIONAL SPACE MULTI-ITEM MODEL-A CASE STUDY OF QIAOJIA LANDSLIDE DEFORMATION OBSERVATION IN JINSHAJIANG. JOURNAL OF ENGINEERING GEOLOGY, 26(s1): 14-21. DOI: 10.13544/j.cnki.jeg.2018040
    Citation: YAO Jiaming, YAO Xin, LIU Xinghong, CHEN Jian, LI Lingjing, ZHOU Zhenkai. 2018: STUDY ON THE ATMOSPHERIC CORRECTION OF D-INSAR REMOVAL BY THREE-DIMENSIONAL SPACE MULTI-ITEM MODEL-A CASE STUDY OF QIAOJIA LANDSLIDE DEFORMATION OBSERVATION IN JINSHAJIANG. JOURNAL OF ENGINEERING GEOLOGY, 26(s1): 14-21. DOI: 10.13544/j.cnki.jeg.2018040

    滑坡D-InSAR观测中的大气误差去除研究以金沙江巧家段为例

    STUDY ON THE ATMOSPHERIC CORRECTION OF D-INSAR REMOVAL BY THREE-DIMENSIONAL SPACE MULTI-ITEM MODEL-A CASE STUDY OF QIAOJIA LANDSLIDE DEFORMATION OBSERVATION IN JINSHAJIANG

    • 摘要: 随着InSAR技术的发展和SAR数据源的丰富,SAR数据相干、配准、轨道误差和地形误差校正等问题已经得到较好地解决,对于大面积观测滑坡这类小范围变形(相对构造运动和地面沉降)非常有效。目前大气相位带来的误差仍然是影响InSAR应用的重要因素。利用空间相关性去除区域低频大气相位延迟是一种无须外部气象数据、简洁高效的方法,但在已有的处理InSAR的商业软件如GAMMA中,大气模型使用的是高程与相位的一次曲线线性模型,无法适应我国西南山区复杂的大气相位湿延迟,往往会引入额外的误差。为此,本文研究了大气相位随高程变化的分布特征和最优拟合函数,并在Matlab软件平台上予以实现,可以将模拟的大气相位从解缠相位中很好地去除,使被大气压制的滑坡形变信息更好地呈现出来。以金沙江河谷巧家段岸坡为研究区,进行了蠕滑变形斜坡的识别验证,验证结果表明使用高程相位拟合多项式比单一线性拟合更易识别出滑坡范围,减少地质灾害隐患点遗漏,这对在我国西南地区水库岸D-InSAR观测滑坡变形的应用具有重要意义。

       

      Abstract: With the development of InSAR technology and the richness of SAR data sources, experts and scholars from various countries have solved the problems of SAR data coherence, registration, orbit error and terrain error correction. It is very effective for observing small-scale deformations such as landslides(relative to tectonic movement and land subsidence).Nowadays, atmospheric phase error is still an important factor affecting InSAR applications. The use of spatial correlation to remove regional low-frequency atmospheric phase delay is a simple and efficient method, and we do not need any external weather data. However, in the existing commercial software for processing InSAR,such as GAMMA,the atmospheric model uses a linear curve model of elevation and phase, which cannot adapt to the complex atmospheric phase wet delay in the southwestern mountainous region of China, and often introduces additional errors. In this paper, I studied the distribution characteristics and optimal fitting function of atmospheric phase with elevation, and implements it on Matlab software platform. In this way, I can remove the simulated atmospheric phase from the unwrapped phase, and make the deformation information of the landslide clearer. We used the bank slope of the Qiaojia section of the Jinsha River Valley as the study area, and performed the identification verification of the creep deformation slope. Result shows that the use of elevation phase fitting polynomial is easier to identify the landslide range than a single linear fit, and reduce the omission of geological disasters. That is of great significance for the observation of landslide deformation on the D-InSAR reservoir bank in southwestern China.

       

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