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Terrestrial Radar Interferometry to Monitor Glaciers with Complex Atmospheric Screen

机译:地面雷达干涉测量技术,用于监测具有复杂大气屏的冰川

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This paper reports the results of two terrestrial surveys aimed at monitoring two Alpine glaciers located in Italy and Spain respectively, and carried out using a Ground Based SAR interferometer. Although the monitoring of glaciers based on this technique does not represent a novelty, these two case studies are peculiar, due to the characteristics of the Alpine glaciers among which the dominant role of the atmospheric phase screen (APS) on the radar signal propagation. These kind of glaciers, with their climate and geographical features, often demand a detailed analysis of the acquired data, at small temporal (less than an hour), and spatial (a few square meters) scale. The meteorological conditions, which affect the dynamics of the glaciers, deeply influenced the backscattering behavior, demanding a careful analysis of the amplitude of the radar signal, to characterize the surface, and of the interferometric phase, to evaluate the role of the APS. Only after the correction of the APS, a final accuracy of a few millimeters/day was attained in the daily velocity of the glacier in both cases.
机译:本文报告了两次地面调查的结果,这些调查旨在分别监测位于意大利和西班牙的两个高山冰川,并使用地面SAR干涉仪进行了调查。尽管基于此技术的冰川监测并不代表新颖性,但由于高山冰川的特征,其中大气相筛(APS)在雷达信号传播中起着主导作用,因此这两个案例研究是独特的。这类冰川具有其气候和地理特征,通常需要在较小的时间范围(不到一个小时)和空间范围(几平方米)上对获取的数据进行详细的分析。影响冰川动力学的气象条件深刻影响了后向散射行为,需要仔细分析雷达信号的振幅,表征表面和干涉相,以评估APS的作用。仅在校正了APS之后,两种情况下冰川的日速度最终都达到了几毫米/天的最终精度。

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