非相关地形上InSAR遥感:持续散射方法

H. Zebker, P. Shankar, A. Hooper
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引用次数: 22

摘要

干涉合成孔径雷达(InSAR)是一种可视的大地测量技术,可以对大范围内的运动进行详细测绘。InSAR仅限于没有太多植被的地区,这使地面免受雷达信号的影响,并使观测到的变形产生随机运动。由此产生的回波“去相关”妨碍了这些区域的精确位移测量。去相关也发生在距离太远的干涉图中。然而,在雷达图像中,某些点(表示为持续散射体)是稳定的,不会去相关,并形成一个基点网络,从而允许在质量较差的干涉图中进行测量。我们推广了一种在自然地形中寻找稳定点网络的算法,而不是在城市地区,并将该方法应用于星载卫星数据。利用现代信息理论来优化持续散射体检测,我们现在可以找到比以前多得多的这样的点。我们已经将这种改进的算法应用于圣安德烈亚斯断层和海沃德断层的旧金山湾段,在这两种情况下,我们都发现在植被区域可以看到大量的稳定点,而这些点迄今为止还无法进行InSAR分析。我们的方法将信息论估计和检测理论整合到方法的各个部分,改进了观测值的识别、滤波和相位展开。确定稳定的真实地面散射点可以绘制细微的地表运动和变形,也可以绘制“裸地”地形。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
InSAR Remote Sensing Over Decorrelating Terrains: Persistent Scattering Methods
Interferometric synthetic aperture radar, or InSAR, is a visual geodetic technique permitting detailed mapping of motion over wide areas. InSAR has been limited to regions without much vegetation, which shields the ground from the radar signals and contributes random motions to the observed deformation. The resulting "decorrelation" of the echoes precludes accurate displacement measurements in these areas. Decorrelation also occurs in interferograms with acquisitions separated too far in the sky. Yet certain points, denoted persistent scatterers, in a radar image are stable, do not decorrelate, and form a network of fiducial points that allow measurements in otherwise poor-quality interferograms. We have generalized an algorithm to find networks of stable points in natural terrain, rather than in urban areas, and applied the method to spaceborne satellite data. Using modern information theory to optimize persistent scatterer detection, we can now find many, many more such points than previously possible. We have applied this improved algorithm to the San Francisco Bay segments of the San Andreas and Hayward faults, and in both cases find that a large number of stable points are seen in the vegetated areas that have to date resisted InSAR analysis. Our method of integrating information theoretic estimation and detection theory to all parts of the method, improves the identification, filtering, and phase unwrapping of the observations. Identification of stable true-ground scattering points permits mapping of subtle surface motions and deformations and also of "bare-Earth" topography.
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