The HF surface wave radar WERA. Part I: Statistical analysis of recorded data

S. Maresca, M. Greco, F. Gini, R. Grasso, S. Coraluppi, N. Thomas
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引用次数: 19

Abstract

Surface wave (SW) over-the-horizon (OTH) radars are not only widely used for ocean remote sensing, but they can also be exploited in integrated maritime surveillance systems. This paper represents the first part of the description of the statistical and spectral analysis performed on sea backscattered signals recorded by the oceanographic WEllen RAdar (WERA) system. Data were collected on May 13th 2008 in the Bay of Brest, France. The data statistical analysis, after beamforming, shows that for near range cells the signal amplitude fits well the Rayleigh distribution, while for far cells the data show a more pronounced heavy-tailed behavior. The causes can be traced in man-made (i.e. radio communications) and/or natural (i.e. reflections of the transmitted signal through the ionosphere layers, meteor trails) interferences.
高频表面波雷达。第一部分:记录数据的统计分析
表面波超视距雷达不仅广泛用于海洋遥感,而且还可用于综合海上监视系统。本文是对海洋韦伦雷达(WEllen RAdar, WERA)系统记录的海洋背散射信号进行统计和频谱分析的第一部分。数据于2008年5月13日在法国布雷斯特湾收集。波束形成后的数据统计分析表明,对于近距离小区,信号幅度很好地符合瑞利分布,而对于远距离小区,数据表现出更明显的重尾行为。其原因可以追溯到人为(即无线电通信)和/或自然(即通过电离层传输信号的反射、流星轨迹)干扰。
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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