模拟无线电高度计回波信号的剖面

M. Borodin
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引用次数: 1

摘要

介绍。无线电高度计用于遥感监测地球和海面,根据信号功率分布,即回波信号功率随时间的依赖关系,在一组探空测量中平均。计算海浪作用下的功率分布需要海面应用的概率分布密度(PDD)信息。现有的PDD模型(线性模型、Gram-Charlier模型和组合模型)在基于信号功率分布评估海面参数时存在一定的缺陷。本文采用非线性Creamer模型对无线电高度计的回波信号进行了模拟。为了验证非线性Creamer模型在海面PDD的有效性,并将其应用于无线电高度计回波信号功率剖面的模拟问题,同时提供了PDD统计参数与风速之间的明确关系。材料和方法。基于线性和非线性Creamer模型,在MATLAB环境下对具有Elfohaily空间谱的有限维二维海面进行了仿真。在3 m/s的小风速值下,非线性Creamer模型形成的海面应用的PDD服从高斯定律。在非线性模式下,无线电高度计回波信号的持续时间随风速的增加平均比线性模式慢5.47%。由于PDD变换,非线性模型回波信号的前沿相对于线性模型的时移可达70 ns,相当于10.5 m。通过对无线电高度计回波信号功率分布的模拟,验证了非线性Creamer模型在获取海面应用PDD时的有效性。在后处理阶段估计无线电高度计回波信号的参数时,可以推荐非线性Creamer模型来模拟回波信号的功率分布,作为输入数据。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Simulating the Profile of a Radio Altimeter Echo Signal
Introduction. Radio altimeters are used for remote monitoring of the Earth and sea surface based on the signal power profile, i.e. the dependence of echo signal power vs time, averaged over a set of sounding measurements. Calculation of the power profile in the presence of sea waves requires information about the probability distribution density (PDD) of sea surface applicates. The existing applicate PDD models (linear, Gram-Charlier, combined model) are characterized by certain drawbacks leading to errors in assessing sea surface parameters based on the signal power profile. In this work, the echo signal of a radio altimeter is simulated using the nonlinear Creamer model for calculating sea surface applicates.Aim. To test the validity of the non-linear Creamer model for obtaining the PDD of sea surface applicates in the problem of simulating the power profile of a radio altimeter echo signal while providing an unambiguous relationship between the statistical parameters of PDD and wind speed.Materials and methods. A two-dimensional sea surface of finite dimensions with an Elfohaily spatial spectrum was simulated in the MATLAB environment based on both linear and non-linear Creamer models.Results. Under small wind speed values of up to 3 m/s, the PDD of sea surface applicates formed by the non-linear Creamer model obey the Gauss law. For the non-linear model, an increase in the duration of an radio altimeter echo signal along with an increase in the wind speed was shown to be 5.47 % slower on average compared to that for the linear model. The time shift of the leading edge of an echo signal for the nonlinear model relative to the linear model due to the PDD transformation may reach 70 ns, which is equivalent to 10.5 m. The conducted study confirmed the validity of the non-linear Creamer model for obtaining the PDD of sea surface applicates when simulating the power profile of a radio altimeter echo signal.Conclusion. The non-linear Creamer model can be recommended for simulating an echo signal power profile for use as input data when estimating the parameters of a radio altimeter echo signal at the stage of post-processing. 
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