3D imaging of an alpine glacier: Signal processing of data from the AlpTomoSAR campaign

S. Tebaldini, F. Rocca, A. Meta, A. Coccia
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Abstract

The ESA field experiment AlpTomoSAR has been planned to investigate the capabilities and potential of L-Band Synthetic Aperture Radar Tomography (TomoSAR) for studying the internal structures of glaciers and ice sheets. The scientific interest in this activity is motivated by the need for improved observations of snow and ice, which are relevant to climate researches and water management. TomoSAR represents today a new potential tool to obtain significant improvements in the capability to characterize natural media from remotely sensed data, providing 3D resolution capabilities of the imaged media. In this paper we present a tomographic analysis of the Mittelbergferner glacier, illuminated during AlpTomoSAR by flying repeatedly along an oval-like racetrack. 3D Single Look Complex cubes were focused for two opposite views by jointly processing all passes in the 3D space, resulting in a spatial resolution cell of about 2 m in all directions. The 3D data cubes were used as a basis for further physical analyses, revealing the presence of scattering elements at few tens of meters below the ice/snow interface.
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高山冰川的三维成像:来自AlpTomoSAR运动数据的信号处理
欧空局计划进行AlpTomoSAR野外实验,以研究l波段合成孔径雷达层析成像(TomoSAR)研究冰川和冰盖内部结构的能力和潜力。对这一活动的科学兴趣是由于需要改进对冰雪的观测,这与气候研究和水管理有关。今天,TomoSAR代表了一种新的潜在工具,可以显著提高从遥感数据中表征自然介质的能力,提供成像介质的3D分辨率能力。在本文中,我们提出了Mittelbergferner冰川的层析分析,在AlpTomoSAR期间,通过沿着椭圆形赛道反复飞行来照亮冰川。通过对三维空间中的所有通道进行联合处理,将三维单视复合立方体聚焦在两个相反的视图上,得到了一个在各个方向上约为2 m的空间分辨率单元。三维数据立方体被用作进一步物理分析的基础,揭示了冰/雪界面下方几十米处散射元素的存在。
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