ERS-1地形测绘与季节雷达干涉测量

H. Zebker, J. Villasenor, S. Madsen
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引用次数: 11

摘要

一种用于地表地形测绘的雷达干涉技术为生成数字高程模型提供了一种高分辨率、全球一致的方法。由于成本和星载硬件复杂性的原因,在几乎重复的轨道上使用单个合成雷达卫星具有吸引力;它还允许从雷达回波的相关特性推断地表的变化。我们用从SEASAT和ERS-1数据生成的地图来说明该技术。我们分析了俄勒冈州森林地区的SEASAT干涉仪图像,其中包括一些没有植被的熔岩流。我们还分析了将该技术应用于从阿拉斯加收集的ERS-1数据生成的地图的预期误差;在撰写本文时,我们还没有生成地图本身。最后,我们概述了一个全球测绘任务的轨道方案。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Topographic Mapping From ERS-1 And Seasat Radar Interferometry
A radar interferometric technique for topographic mapping of sur- faces promises a high resolution, globally consistent approach to gen- eration of digital elevation models. Utilizing a single synthetic aper- ture radar satellite in a nearly repeating orbit is attractive for cost and spaceborne hardware complexity reasons; also it permits infer- ence of changes in the surface from the correlation properties of the radar echoes. We illustrate the technique with maps generated from SEASAT and ERS-1 data. We have analyzed a SEASAT interferomet- ric image of a forested area in Oregon which includes some unvegetated lava flows. We also present an analysis of errors expected from appli- cation of the technique to maps generated from ERS-1 data collected over Alaska; as of the time of this writing we have not yet generated the maps themselves. Finally we outline an orbital scenario for a global mapping mission.
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