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Validation of Sea-Ice Topographic Heights Derived From TanDEM-X Interferometric SAR Data With Results From Laser Profiler and Photogrammetry

机译:验证TanDEM-X干涉SAR数据得出的海冰地形高度以及激光轮廓仪和摄影测量的结果

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摘要

In this paper, the retrieval of sea-ice surface heights from the interferometric TanDEM-X data is investigated. The data were acquired over fast and drifting ice in Fram Strait located between Greenland and Svalbard. Additional measurements of the sea-ice surface topography were carried out using a stereo camera and a laser altimeter. The comparison of the surface elevation retrieved from TanDEM-X imagery with the results of the stereo camera measurements revealed that sea-ice ridges greater than 0.5 m can be estimated with a root-mean-square error of 0.3 m or less with the error decreasing as a function of ridge height. Although the helicopter-borne laser data are only available as 1-D profiles with a much higher across-track spatial resolution than the TanDEM-X data, they proved to be useful for the validation. The need for multilook averaging to reduce the phase noise is identified as the main challenge in achieving the spatial resolution necessary for retrieving sea-ice surface topography using synthetic aperture radar interferometry.
机译:本文研究了从干涉TanDEM-X数据中获取海冰表面高度的方法。数据是通过格陵兰岛和斯瓦尔巴特群岛之间的弗拉姆海峡的快速流动冰层获得的。使用立体相机和激光测高仪对海冰表面形貌进行了其他测量。从TanDEM-X图像中检索到的表面高程与立体相机测量结果的比较表明,可以估计大于0.5 m的海冰脊,且均方根误差为0.3 m或更小,且误差减小作为山脊高度的函数。尽管直升飞机上的激光数据仅以1-D轮廓形式提供,其跨轨道空间分辨率比TanDEM-X数据高得多,但事实证明它们对验证很有用。为了降低使用合成孔径雷达干涉法获取海冰表面形貌所必需的空间分辨率,对降低相位噪声的多视场平均的需求已被确定为主要挑战。

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