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Statistical combination of attenuations by multiple atmospheric effects

机译:多种大气效应对衰减的统计组合

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At frequencies above 10 GHz, traditional techniques for estimating losses due to atmospheric effects focus on the dominant source of fading, rain attenuation. An approach different from the traditional procedure for calculating attenuation in considered in this paper. Distributions of attenuation were derived for a theoretical system operating in the Washington, D.C. area with a frequency, f=27.505 GHz and elevation angle, /spl theta/=20.0/spl deg/. Local rain rates were used in conjunction with the global model to create a cumulative distribution function (CDF) of rain attenuation. A mean attenuation due to gaseous absorption was then calculated using MPM 93 (Liebe, 1993) using mean local temperature and relative humidity. Vertical variation in absolute humidity along the path was accounted for using average profiles (Slobin, 1981). The result was summed with the CDF of rain attenuation to produce a statistical distribution of rain attenuation.
机译:在高于10 GHz的频率下,传统技术用于估算由于大气效应引起的损失,重点关注衰落,雨衰减。一种不同于本文考虑衰减的传统程序的方法。导出衰减的分布对于在华盛顿州,D.C.的理论系统,D.C.区域,频率为F = 27.505 GHz和仰角,/SPLθ/ = 20.0 / SPL°/。本地雨率与全球模型结合使用,以创造雨衰的累积分布函数(CDF)。然后使用MPM 93(Liebe,1993)使用平均局部温度和相对湿度来计算由于气态吸收引起的平均衰减。沿着路径的绝对湿度的垂直变化被占使用平均曲线(1981)。结果总结了雨衰减的CDF,以产生雨衰减的统计分布。

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