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Applications and development of new algorithms for displacement analysis using InSAR time series.

机译:使用InSAR时间序列进行位移分析的新算法的应用和开发。

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摘要

Time series analysis of Synthetic Aperture Radar Interferometry (InSAR) data has become an important scientific tool for monitoring and measuring the displacement of Earth's surface due to a wide range of phenomena, including earthquakes, volcanoes, landslides, changes in ground water levels, and wetlands. Time series analysis is a product of interferometric phase measurements, which become ambiguous when the observed motion is larger than half of the radar wavelength. Thus, phase observations must first be unwrapped in order to obtain physically meaningful results. Persistent Scatterer Interferometry (PSI), Stanford Method for Persistent Scatterers (StaMPS), Short Baselines Interferometry (SBAS) and Small Temporal Baseline Subset (STBAS) algorithms solve for this ambiguity using a series of spatio-temporal unwrapping algorithms and filters. In this dissertation, I improve upon current phase unwrapping algorithms, and apply the PSI method to study subsidence in Mexico City.;PSI was used to obtain unwrapped deformation rates in Mexico City (Chapter 3),where ground water withdrawal in excess of natural recharge causes subsurface, clay-rich sediments to compact. This study is based on 23 satellite SAR scenes acquired between January 2004 and July 2006. Time series analysis of the data reveals a maximum line-of-sight subsidence rate of 300mm/yr at a high enough resolution that individual subsidence rates for large buildings can be determined. Differential motion and related structural damage along an elevated metro rail was evident from the results. Comparison of PSI subsidence rates with data from permanent GPS stations indicate root mean square (RMS) agreement of 6.9 mm/yr, about the level expected based on joint data uncertainty. The Mexico City results suggest negligible recharge, implying continuing degradation and loss of the aquifer in the third largest metropolitan area in the world.;Chapters 4 and 5 illustrate the link between time series analysis and three-dimensional (3-D) phase unwrapping. Chapter 4 focuses on the unwrapping path. Unwrapping algorithms can be divided into two groups, path-dependent and path-independent algorithms. Path-dependent algorithms use local unwrapping functions applied pixel-by-pixel to the dataset. In contrast, path-independent algorithms use global optimization methods such as least squares, and return a unique solution. However, when aliasing and noise are present, path-independent algorithms can underestimate the signal in some areas due to global fitting criteria. Path-dependent algorithms do not underestimate the signal, but, as the name implies, the unwrapping path can affect the result. Comparison between existing path algorithms and a newly developed algorithm based on Fisher information theory was conducted. Results indicate that Fisher information theory does indeed produce lower misfit results for most tested cases.;Chapter 5 presents a new time series analysis method based on 3-D unwrapping of SAR data using extended Kalman filters. Existing methods for time series generation using InSAR data employ special filters to combine two-dimensional (2-D) spatial unwrapping with one-dimensional (1-D) temporal unwrapping results. The new method, however, combines observations in azimuth, range and time for repeat pass interferometry. Due to the pixel-by-pixel characteristic of the filter, the unwrapping path is selected based on a quality map. This unwrapping algorithm is the first application of extended Kalman filters to the 3-D unwrapping problem.;Time series analyses of InSAR data are used in a variety of applications with different characteristics. Consequently, it is difficult to develop a single algorithm that can provide optimal results in all cases, given that different algorithms possess a unique set of strengths and weaknesses. Nonetheless, filter-based unwrapping algorithms such as the one presented in this dissertation have the capability of joining multiple observations into a uniform solution, which is becoming an important feature with continuously growing datasets.
机译:合成孔径雷达干涉术(InSAR)数据的时间序列分析已成为监测和测量由于地震,火山,滑坡,地下水位变化和湿地等多种现象而引起的地球表面位移的重要科学工具。 。时间序列分析是干涉式相位测量的产物,当观察到的运动大于雷达波长的一半时,相位测量将变得模棱两可。因此,相位观测必须首先被解开以获得物理上有意义的结果。持久散射体干涉法(PSI),斯坦福方法用于持久散射体(StaMPS),短基线干涉法(SBAS)和小时基基线子集(STBAS)算法使用一系列时空解缠算法和滤波器来解决这种歧义。本文对现有的相位解缠算法进行了改进,并应用PSI方法研究了墨西哥城的沉降。第三章,利用PSI获得墨西哥城的解缠变形率,即地下水抽取量超过自然补给量。导致地下富含粘土的沉积物致密。这项研究基于2004年1月至2006年7月之间采集的23个卫星SAR场景。对数据的时间序列分析显示,最大的视线沉降速率为300mm / yr,且分辨率足够高,大型建筑物的个体沉降速率可以达到。被确定。结果表明,沿升高的地铁轨道的差速运动和相关的结构破坏是显而易见的。将PSI沉降率与来自永久性GPS站的数据进行比较,得出的均方根(RMS)一致性为6.9 mm / yr,大约是基于联合数据不确定性所期望的水平。墨西哥城的结果表明补给量可以忽略不计,这意味着世界第三大都市区含水层的持续退化和损失。第4章和第5章说明了时间序列分析与三维(3-D)相展开之间的联系。第4章重点介绍了展开路径。展开算法可以分为两组,分别是路径相关算法和路径独立算法。路径相关算法使用局部展开功能,逐个像素应用于数据集。相反,与路径无关的算法使用全局优化方法(例如最小二乘法),并返回唯一的解决方案。但是,当存在混叠和噪声时,由于全局拟合标准,与路径无关的算法可能会在某些区域低估信号。依赖于路径的算法不会低估信号,但是,顾名思义,展开路径会影响结果。比较了现有路径算法和基于Fisher信息理论的最新算法。结果表明,费舍尔信息理论确实在大多数测试情况下确实产生了较低的失配结果。现有的使用InSAR数据生成时间序列的方法采用特殊的滤波器,以将二维(2-D)空间展开与一维(1-D)时间展开结果结合在一起。但是,新方法将方位角,范围和时间的观测结果结合在一起,以进行重复通过干涉测量。由于滤波器的逐像素特性,因此根据质量图选择展开路径。这种展开算法是扩展卡尔曼滤波器在3-D展开问题中的首次应用。InSAR数据的时间序列分析被用于具有不同特征的各种应用中。因此,鉴于不同的算法具有独特的优点和缺点,很难开发出一种在所有情况下都能提供最佳结果的算法。但是,基于滤波器的解包算法(如本论文中提出的算法)具有将多个观测值合并为统一解的能力,这在数据集不断增长的情况下正成为一项重要功能。

著录项

  • 作者

    Osmanoglu, Batuhan.;

  • 作者单位

    University of Miami.;

  • 授予单位 University of Miami.;
  • 学科 Geophysics.;Remote Sensing.
  • 学位 Ph.D.
  • 年度 2011
  • 页码 163 p.
  • 总页数 163
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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