相干脉冲海杂波回波多尺度分析的应用

G. Davidson, H. Griffiths, R. Anderson
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引用次数: 2

摘要

海杂波在低掠射角度下的变异性对正确的振幅统计模型产生了分歧。如果散射机制是非平稳的,则利用现有的平稳理论识别相关区域是一种方法。连续小波变换应用于相干脉冲数据表明,海面散射事件可以是离散的,并以不同的形式出现。给出了波速谱随时间变化的结果。这最终为我们提供了一个速度范围内的二阶统计量,使我们能够根据观察到的事件的时频长比,在杂波速度下提出目标检测策略。测量变换中最大值的持久性允许在不设置幅度阈值的情况下检测杂波水平。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Application of multiscale analysis to coherent pulsed sea clutter returns
The variability of sea clutter when viewed at low grazing angles has divided opinion upon the correct model for the amplitude statistics. If the scattering mechanism is non-stationary then a method of utilising existing stationary theory is to identify correlated regions. The continuous wavelet transform applied to coherent pulsed data demonstrates that scattering events from the sea surface can be discrete and occur in different forms. Results are presented to show the varying wave velocity spectrum as a function of time. This ultimately gives us second order statistics over a range of velocities which allows us to propose a target detection strategy at clutter velocities, based on the time frequency aspect ratio of the observed event. Measuring the persistence of maxima in the transform allows detection below the clutter level without setting an amplitude threshold.
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