WSM干涉法监测大地震变形的研究

Ting-chen Jiang, Tao Li, Jing-nan Liu
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引用次数: 1

摘要

宽条模式(Wide Swath mode, WSM)又称扫描成像(ScanSAR),其特点是合成孔径时间由周边子条共享,降低了方位角分辨率,从而实现了对地震的大面积变形监测。由于成像原理不同,干涉测量过程中存在相干性、共配准、大气效应校正、大地水准面起伏等诸多差异。为了利用扫描sar数据获得更广阔的变形场,本文对扫描sar干涉测量的关键技术进行了研究和分析。最后利用ENVISAT ScanSAR数据获得了汶川和玉田地震405 km ×405 km形变场。该方法在汶川和玉田地震中的应用,对大地震和地壳运动等地学研究具有重要意义。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Research on deformation monitoring caused by large earthquake with WSM interferometry
Wide Swath mode (WSM) is also called as ScanSAR, it is character is that synthetic aperture time is shared by circumjacent sub swaths and azimuth resolution is reduced so that large area deformation monitoring for earthquakes is realized. For imaging principle ScanSAR and IM mode are different, process of interferometry also have a lot of dissimilitudes such as coherence, co-registering, correction of atmosphere effects and geoid undulation. In order to make use of ScanSAR data to get wider deformation field, key techniques of ScanSAR interferometry are studied and analyzed in this paper. In the end, 405 km ×405 km deformation fields of Wenchuan and Yutian earthquake are gained by using ENVISAT ScanSAR data. With the application to ScanSAR interferometry in Wenchuan and Yutian earthquake, it is significant for Earth Science research such as large earthquakes and crustal motion.
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