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Analysis of sea spikes in radar sea clutter data

机译:雷达海杂波数据中的海峰分析

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In this paper three sets of high-resolution, coherent, and polarimetric radar sea clutter data are analyzed and compared with radar sea clutter models. The nature of the data allows a thorough analysis of the power, polarization and velocity of the sea clutter. It is shown that these quantities, especially the velocity, are good measures of many physical properties of the ocean surface. Furthermore, it is shown that these physical properties match well with the sea clutter models. Sea clutter is found to consist of two components, a diffuse background, characterized by low values of backscattered power, HH/VV polarization ratio and Doppler velocity, and a number of spiking events, which possess higher power, polarization ratio and velocity. The background is reasonably well modeled by tilt-modulated Bragg scattering, whereas the spikes may be associated with the scattering on steepened and/or breaking waves. Moreover, it is shown that the influence of microbreakers has to be taken into account to explain the relatively high polarization ratio. A breaking wave origin for the spikes is supported in two ways. First, by a detailed analysis of the temporal behavior of individual spike backscatter properties, and second, by a statistical analysis of the entire population of spikes.
机译:本文分析了三组高分辨率,相干和极化雷达海杂波数据,并与雷达海杂波模型进行了比较。数据的性质允许对海杂波的功率,极化和速度进行全面分析。结果表明,这些量,尤其是速度,是衡量海洋表面许多物理性质的良好方法。此外,表明这些物理性质与海杂波模型很好地匹配。发现海杂波由两个部分组成,一个是漫射背景,其特征在于反向散射功率,HH / VV极化比和多普勒速度的值较低,以及一些峰值事件,它们具有较高的功率,极化比和速度。通过倾斜调制的布拉格散射可以很好地模拟背景,而尖峰可能与陡峭和/或破碎波上的散射有关。此外,已经表明,必须考虑微断路器的影响来解释相对较高的极化率。尖峰的碎波起源有两种支持方式。首先,通过详细分析各个峰值后向散射特性的时间行为,其次,通过对整个峰值总数进行统计分析。

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