A phenomenological model for radar signal propagation in evaporation ducts

G. Fedele, P. Lombardo, D. Deli
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Abstract

A phenomenological model is proposed for the propagation of wideband radar pulses through an evaporation duct. The proposed model extends the previous models in two directions: (i) it presents a wideband characterization, thus removing the continuous wave hypothesis of most previous models; (ii) it fully considers the random characteristic of the geometric parameters by providing a statistical model. In particular, a statistical approach is used for the description of the rough sea surface due to the presence of wind and sea swells. The resulting model describes the duct as a random Gaussian fading channel with statistical parameters related to the surface geometrical characteristics. Both the single point statistic of the received signals and the spectral distortion of the transmitted pulses are studied by the proposed model. In particular, the coherence bandwidth is shown to depend essentially on the ratio between the surface standard deviation and the correlation length, i.e., on the local surface slope. As expected, the channel bandwidth decreases as either the sea roughness increases (larger standard deviation) or the surface decorrelates. These results apply both to TE and TM modes and both to exponential and Gaussian models assumed to describe the spatial correlation function of the surface heights.
雷达信号在蒸发管道中传播的现象学模型
提出了宽带雷达脉冲通过蒸发导管传播的现象模型。本文提出的模型在两个方面扩展了以前的模型:(1)它提出了宽带特性,从而消除了大多数以前模型的连续波假设;(ii)通过提供统计模型,充分考虑几何参数的随机特性。特别地,统计方法被用于描述由于风和海浪的存在而产生的粗糙海面。所得模型将管道描述为随机高斯衰落通道,其统计参数与表面几何特性相关。利用该模型研究了接收信号的单点统计量和发射脉冲的频谱畸变。特别是,相干带宽主要取决于表面标准差与相关长度之间的比值,即取决于局部表面斜率。正如预期的那样,信道带宽随着海面粗糙度的增加(较大的标准偏差)或海面去相关而减小。这些结果既适用于TE模式和TM模式,也适用于描述地表高度空间相关函数的指数模型和高斯模型。
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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