Modeling and simulation of sea surface radar observations

A. Ghaleb, S. Even, R. Garello, B. Chapron, N. Pinel, N. de Beaucoudrey, F. Comblet, M. Parenthoen, E. Pottier
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引用次数: 5

Abstract

This paper describes a methodology to model and simulate the reflectivity measured by radar observing a maritime environment. The simulation principle consists of reproducing the acquisition of a Real Aperture Radar (RAR) moving along its axis. Pulse after pulse, high range resolution profiles are successively computed by summing the contribution of backscatters comprised in the radar footprint. The scatterer contributions are calculated from typical statistical distribution estimation. The simulation output, called raw data, is the concatenation of time profiles (short time) successively obtained for each radar pulse (long time). A SAR algorithm is then applied in order to form a high resolution image. The generation of the sea surface is achieved by a multi-scale model. This approach takes into account phenomena at different scales (from long wave to small objects), all in interaction in a hydrodynamic environment. It is thus possible to focus locally on contributions considered as more significant. To improve the processing time some contributions can also be retrieved from Look-Up Tables. Hence, our method performs a realistic simulation of electromagnetic interactions in a maritime environment.
海面雷达观测的建模和模拟
本文介绍了一种模拟和模拟海洋环境雷达反射率的方法。仿真原理包括再现真实孔径雷达(RAR)沿其轴线运动的捕获。通过对雷达足迹中的后向散射体的贡献求和,连续计算出一个又一个脉冲的高距离分辨率轮廓。根据典型的统计分布估计计算散点贡献。模拟输出称为原始数据,是对每个雷达脉冲(长时间)先后获得的时间曲线(短时间)的串联。然后应用SAR算法形成高分辨率图像。海面的生成是通过一个多尺度模型来实现的。这种方法考虑了不同尺度(从长波到小物体)的现象,所有这些现象都在水动力环境中相互作用。因此,可以在当地集中注意被认为更重要的捐款。为了缩短处理时间,还可以从查找表中检索一些贡献。因此,我们的方法对海洋环境中的电磁相互作用进行了逼真的模拟。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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