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A new method for analyzing the attenuation characteristics of satellite radar altimeter signals due to rainfall based on a multilayer medium model

机译:一种新方法,用于分析卫星雷达高度计信号引起的降雨基于多层介质模型的降雨

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摘要

Rainfall has an attenuation of backscatter coefficient of the sea surface and a change in the sea surface roughness, and these effects give rise to some errors in retrieving the sea surface wind speed, the significant wave height, and wave slope. It is meaningful to make considerable efforts to study the attenuation of radio waves caused by rainfall. In this article, a new model of analyzing the attenuation characteristics of satellite radar altimeter pulse signals because of rainfall is presented. First, the model of the equivalent permittivity of rainfall is calculated and presented. The imaginary part of the equivalent permittivity is studied when radio frequency and rainfall rate vary, respectively. Second, a new theoretical model and method of analyzing the effect of rainfall on satellite radar altimeter pulses is presented based on a multilayer-medium model with the equivalent permittivity of rainfall. On the other hand, some existing models of computing rainfall attenuation characteristics of radar signals are studied and improved to some extent. Finally, some attenuation characteristics of radar signals due to rainfall are calculated by those models. The calculated results show that the attenuation characteristics of radar altimeter pulse signals are all in good agreement with those by other models. The results computed by the multilayer-medium model can provide a good theoretical explanation and understanding for these attenuation characteristics of radar pulse signals and can also give some data support and corrections for the measured oceanic parameters by the satellite radar altimeter.
机译:降雨具有海面的后散射系数和海面粗糙度的变化,并且这些效果引起了在检索海面风速,显着波浪高度和波坡方面的一些误差。做出大量努力研究由降雨引起的无线电波的衰减是有意义的。在本文中,提出了一种新模型,分析了由于降雨而分析卫星雷达高度计脉冲信号的衰减特性。首先,计算并呈现降雨量等同介电常数的模型。当射频和降雨率分别变化时,研究了等效介电常数的虚部。其次,基于具有等同介电常数的多层介质模型,提出了一种新的理论模型和分析降雨量对卫星雷达高度计脉冲的影响。另一方面,在一定程度上研究并改善了一些现有的计算降雨衰减特性的计算雷达信号的衰减特性。最后,通过降雨导致的雷达信号的一些衰减特性由这些模型计算。计算结果表明,雷达高度计脉冲信号的衰减特性与其他模型的响应均匀。多层介质模型计算的结果可以为雷达脉冲信号的这些衰减特性提供良好的理论解释和理解,并且还可以通过卫星雷达高度计提供一些数据支持和测量的海洋参数的校正。

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