分层介质中冰探数据图像频谱分解的反投影算法

Chengfeng Lv, T. Hao
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引用次数: 0

摘要

合成孔径雷达成像可以虚拟地观测场景并沿预定轨迹识别目标,可应用于时域冰探数据,以较少的副瓣杂波绘制冰下地形结构。但分层介质中复杂的信号传输路径限制了聚焦的效率和精度。本文提出了在谱域对分层介质中多路径形成的组合矢量进行分解来分析波数支持域的方法。这有助于确定最低的奈奎斯特采样率,从本质上加快了无混叠图像的重建,并且可以固有地插入到基于分治方案的快速分解反投影算法框架中,递归地生成从低到高质量的图像。利用这种技术,飞行的沿轨道运动扰动和未知的断层扫描变化,可以在额外的但可忽略的计算费用中得到适应。最后给出了南极测冰实测数据的结果,验证了该方法的良好性能。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Image Spectrum Decomposition of Ice-Sounding Data in Stratified Medium for Back Projection Algorithm
Image formation of synthetic aperture radar, which virtually observes the scenes and identifies targets along the predetermined trajectory, can be applied to ice-sounding data in the time domain, to map subglacial topographic structures with less sidelobe clutters. However, complex signal transmission path within stratified media limits the efficiency and accuracy of focusing. Here, we present the method to analyze the wavenumber support region by decomposing in the spectrum domain the combined vector formed from multi-paths in stratified media. This assists to determine the lowest Nyquist sampling rate, which essentially accelerates the reconstruction of aliased-free images and can be inherently inserted into the fast factorized back projection algorithm framework, based on divide-and-conquer scheme, recursively yielding low-to-high quality images. With this technique, along-track motion perturbations of flights and unknown tomography variations, can be accommodated at the additional but neglectable computational expenses. Results from real ice-sounding data in Antarctica are presented to validate the promising performance of the proposed method.
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