融合升降轨SAR干涉相位和幅度信息揭示地表三维形变场的研究
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摘要
针对InSAR技术只能监测地表在雷达视线方向上的形变的缺点,详细介绍了融合升降轨SAR干涉相位和幅度信息监测地表三维形变的具体方法.该方法主要分为3个步骤:(1)利用升降轨SAR干涉相位监测地表在2个不同雷达视线方向上的形变;(2)利用升降轨SAR幅度信息获取地表在2个不同方位向上的形变;(3)采用最小二乘准则和Helmert方差分量估计融合上述4个不同方向的形变,从而估计地表三维形变场.以2003年伊朗Bam地震为例,应用该方法成功地揭示了该地震引起的地表三维形变场,结果显示Bam地区北部出现了明显地表下沉和沿近西南方向的水平运动,而南部则出现地表隆起和沿近东南方向的水平运动.上下、南北和东西3个方向上的地表形变场都很好地吻合了地震断层所在的位置,最大形变量分别达22,40和30cm.最后,将此三维形变场与利用Okada模型模拟的三维形变场进行了比较,证明了该方法能够得到可靠且精度较高的地表三维形变场.
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