Heterogeneous surface displacement pattern at the Hatchobaru geothermal field inferred from SAR interferometry time-series     

《International Journal of Applied Earth Observation and Geoinformation》2016

We estimated surface displacements using persistent scatterer SAR interferometry (PS-InSAR) around the Hatchobaru geothermal field, Japan, from 18 ALOS/PALSAR images acquired from July 2007 to December 2010. Generally, geothermal fields, covered with natural targets such as rocky terrain and vegetation, have been one of the difficult targets for PS-InSAR analysis. However, we applied space adaptive filtering to increase the number of pixels for measuring surface displacement. The results of our analysis demonstrate ground subsidence with decaying velocity over the observation period around the geothermal field. The spatial pattern of ground subsidence includes sharp boundaries of subsidence that can be interpreted as fault traces. We demonstrated the usefulness of PS-InSAR analysis with the space adaptive filtering to estimate surface displacements with high spatial resolution and high spatial density around a geothermal field.  相似文献   

Resolution of prominent crustal scatterers near the Noress small-aperture array     

Michael A. H. Hedlin  Jean-Bernard Minster  John A. Orcutt 《Geophysical Journal International》1994,119(1):101-115

  相似文献   

利用DS-InSAR技术监测黄河三角洲地表形变     

曹建涛  郑翔元  范洪冬  李国华  黄晨 《大地测量与地球动力学》2022,42(11):1177-1183

针对黄河三角洲地区湿地及农田多、范围大,导致PS-InSAR技术难以获取高密度地表形变信息的问题,提出一种基于分布式目标InSAR（DS-InSAR）的黄河三角洲地表形变监测方法。该方法通过置信区间估计选取同质像元点,利用特征值分解方法计算主散射体对应相位值以达到相位优化的目的,再根据时空相干性确定分布式目标,最后建模解算时序地表形变信息。以26景Sentinel-1A影像为数据源,提取2019-12～2020-12期间黄河三角洲地区的地表沉降信息,与PS-InSAR方法结果相比,点位密度提高5.56倍;两种方法获取的同名点对形变速率的相关系数为0.727,说明两者具有很好的一致性。实验结果表明,研究区内存在4处明显沉降区域,最大沉降速率达-238 mm/a,经分析及实地调查验证,其主要影响因素为地下卤水及油气开采。  相似文献   

PS-DInSAR公共主影像的优化选取   总被引：8，自引：1，他引：7  

陈强  丁晓利  刘国祥 《测绘学报》2007,36(4):395-399

在充分顾及DInSAR时空基线跨度及多普勒质心频率差异3个因素对干涉相关性影响的基础上,提出一种PS—DInSAR公共主影像的优化选取算法,采用综合相关测度作为总体干涉相关性的衡量指标,给出具体的综合相关函数模型及其求解方法。借助欧洲空间局（ESA）ERS-1／2卫星从1992—2002年间飞越上海地区所获取的25幅C波段SAR影像作为源数据,开展了PS—DInSAR公共主影像的优化选取实验。计算结果与分析表明,综合相关系数模型用于PS公共主影像的优化选取是有效的和可靠的。  相似文献   

参照标准点探测PS法     

易辉国  张磊  李宁  熊文秀  许兵 《大地测量与地球动力学》2015,35(4):684-687

提出参照标准点探测PS法。既考虑PS的强散射特性,又顾及其稳定性,且初选时振幅阈值的设置参照每景影像中PS标准点的振幅值,精选时振幅离差阈值的设置也参照这些PS标准点的振幅离差值,都不需要人工设定。选取澳门半岛为实验区,以18景TerraSAR-X为数据源,进行PS探测实验。结果表明,相比于传统的PS探测方法,本方法能更快速、有效、可靠地探测出SAR影像中的PS。  相似文献   

极化SAR影像弱散射地物统计分类   总被引：2，自引：1，他引：1  

赵伶俐  杨杰  李平湘  郎丰铠  史磊 《遥感学报》2013,17(2):306-319

针对Wishart分类器对功率具有较强的依赖性, 不易区分极化SAR影像上水体、道路、裸土、阴影等弱后向散射地物的问题, 提出一种利用极化目标分解和假设检验的弱散射地物统计分类方法。即在H-α初始化的基础上, 使用似然比检验得出像元与每个类中心的相似性, 并将其作为像元与类中心的距离测度。根据第一类错误概率和统计量的概率分布, 将相似性很小的强散射点归为拒绝类, 减少对分类的影响;对不能显著拒绝的像元归入具有最小统计量的类别中。通过使用E-SAR L波段和Radarsat-2 C波段全极化数据进行实验, 结果表明本文方法有利于弱散射地物极化信息的利用, 能够实现水体、道路、裸露的土壤和阴影等的精确分类。  相似文献   

融合分布式目标的小基线集干涉测量方法应用     

殷幼松  张永红  吴宏安  康永辉 《测绘科学》2017,42(7)

针对在地理国情监测项目中遇到的时间序列InSAR技术获取的地表形变结果存在空间采样率不足的现状,该文以传统小基线集干涉测量方法为基础,融合分布式目标提取地表缓慢形变信息。以TerraSAR-X星载SAR SLC影像为数据源,对融合后的方法进行验证,获取了研究区域时间序列地表平均形变速率。结果表明,融合分布式目标的小基线集算法可以有效提高监测区域地表形变信息的获取,在非城市地区及传统方法不能提取高相干稳定点目标的区域克服了原有方法的缺点,表现出了很好的适用性。  相似文献   

福建省泉州地区断裂带地壳形变PS-InSAR监测          下载免费PDF全文

田福金  郭建明 《地震工程学报》2015,37(1):196-201

PS-InSAR技术能够有效降低常规差分干涉雷达受时间失相干、空间失相干和大气效应的影响,在常规D-InSAR不能形成干涉条纹的情况下,可利用时间序列的雷达影像和相位稳定的永久散射体目标点获取离散的PS像素点形变速率。以福建省泉州地区的断裂带为研究对象,对1996-1999年的22景ERS SAR数据进行PS-InSAR处理,得出研究区主要断裂的视线向位移速率为3~5mm/a,表明该区断裂仍有一定的活动性,具有潜在的地震危险。  相似文献   

永久散射体差分干涉测量技术中SAR影像精配准的一种新方法     

陶秋香  刘国林 《测绘学报》2012,41(1):69-0

提出并实现了一种基于加权最小二乘的低相干SAR像对精配准新方法。该方法借助一幅与主、辅影像相干性都较高的第三幅影像来完成低相干SAR影像对的初步配准,利用加权最小二乘法求出二者间的坐标映射函数,从而快速高效地实现低相干SAR影像对的高精度亚像元级配准。采用ERS-1/2实际数据的配准实验,验证了该方法可以提高低相干SAR像对的干涉图质量,提高二者之间的相干性和控制点的配准精度,改善低相干SAR影像对的配准效果,在一定程度上解决了PS InSAR技术中低相干SAR影像对的配准问题。  相似文献   

Changes in the early part of the seismic coda due to localized scatterers: The estimation ofQ in a stope environment     

A. Cichowicz  R. W. E. Green 《Pure and Applied Geophysics》1989,129(3-4):497-511

A single scattering model was used to analyse the temporary changes in the mean density of scattered waves in a discrete random medium. The model of the mean energy density, originally proposed bySato (1977) for spherical radiation and isotropic scattering, has been modified and applied to a medium in which the scatterers are confined to a specified volume. The time variation of the early part of the mean energy density function for the different source durations was investigated. The dominant effect on the theoretical mean energy density is caused by the specified volume containing scatterers. The duration of the source pulse influences the early part of the coda fort/t ₀<1.2, wheret is the lapse time measured from the source origin time, andt ₀is arrival time of the body wave.The analysis of the coda signal of micro-events occurring immediately in front of the face enables us to estimate the size of the fracture zone induced by the stope. The model of the mean energy density of coda for a medium containing scatterers close to the seismic source was used to analyse a large number of events recorded close to an advancing mine face in a deep level gold mine in South Africa. The coda decay rate has two trends: the first, with a steep decay of coda, is produced by a larger deviation of rock parameters and/or larger size of the scatterers; the second trend, which decays more slowly, has the corresponding mean-free path ranging from 20 m to 200 m. The analysis indicates that the rock mass about 15–20 m from the stope contains a large proportion of fractured and blocked rock, which is the source of scattering. The scattering of theS-wave was much stronger and more stable, with the mean-free path varying from 11 m to 45 m. This is due to the shorter wavelength of theS wave in comparison with theP wave. The quality factor for theP coda wave varies from 30 to 100 in the fracture zone of stope and outside this zone it has a value of 300. The quality factor of theS wave varies from 20 to 78 in the equivalent volume. For rock surrounding the stope the ratioQ _sp ^–1 /Q _ss ^–1 varied from 0.31 to 0.69. This suggests that the radii of scatterers are smaller than 3.5 m.  相似文献