合成孔径雷达干涉测量原理与应用

被引：16

作者：

游新兆

乔学军

王琪

杜瑞林

机构：

[1] 中国地震局地震研究所

来源：

大地测量与地球动力学 | 2002年 / 03期

关键词：

合成孔径雷达干涉; 原理; 数字高程模型; 地表形变;

D O I：

10.14075/j.jgg.2002.03.027

中图分类号：

P225.1 [无线电测距];

学科分类号：

摘要：

合成孔径雷达 (SAR)是一种微波相干成像方法 ,应用不同波段的雷达信号可以对地球表面不同的散射特性成像。合成孔径雷达干涉 (InSAR)是将两个不同轨道位置或不同时间获得的复数SAR数据进行相位差分处理 ,从这些差分干涉数据中可以提取特别有用的信息 ,用于绘制地形图 ,测量诸如地震、火山、冰川运动等造成的地形变 ,研究植被覆盖特性、洋流等。介绍了InSAR的基本原理与应用 ,并对影响干涉结果的一些重要因素进行了分析。

引用

页码：109 / 116

页数：8

共 24 条

[1]

Crossed orbit interferometry: Theory and experimental results from SIR-B. Gabriel A K and Goldstein R M. International Journal of Remote Sensing . 1988

[2]

Analysis of coseismic surface displacement gradients using radar interferometry:new insights into the Landers earthquake. Peltzer G,Hudnut K and Feigl K. Journal of Geophysical Research . 1994

[3]

Satellite radar interferometry: Two-dimensional phase unwrapping. Goldstein R M,Zebker H A and Werner C L. Radio Science . 1988

[4]

GPS results of current crustal movement of china continent and primary analysis. You Xinzhao,Du Ruilin,et al. Crustal Deformation and Earthquake . 2001

[5]

Detection of subsurface features in Seasat radar images of Means Valley, Mojave Desert, California. Blom R,Crippen R E and Elachi C. The Journal of Geology . 1984

[6]

InSAR Investigation in the Early Stage of the Three Gorges Project. You Xinzhao,Li Shusun,et al. Crustal Deformation and Earthquake . 2001

[7]

Topographic mapping from interferometric synthetic aperture radar observations. Zebker H A and Goldstein R M. Journal of Geophysical Research . 1986

[8]

Satellite radar interferometry for monitoring ice sheet motion: application to an Antarctic ice stream. Goldstein R M,Engelhardt H,Kamb B,et al. Science . 1993

[9]

Deflation of Mount Etna monitored by spaceborne radar intererometry. Massonnet D,Briole P and Arnaud A. Nature . 1995

[10]

Accuracy of topographic maps derived from ERS - 1 interferometric radar. Zebker H A,Werner C L,Rosen P A,et al. IEEE Transactions on Geoscience and Remote Sensing . 1994

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