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Raindrop size distribution using method of moments for terrestrial and satellite communication applications in Singapore

机译:在新加坡的地面和卫星通信应用中,采用矩量法分配雨滴大小

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摘要

As communication services using higher frequencies are growing rapidly in the tropics, there is an increasing need for a finer model to predict the attenuation due to rain. The raindrop size distribution (DSD) is one of the major sources of error in any prediction model, mainly because of its variability in both space and time. The DSD parameters are computed from distrometer data that are classified into stratiform and convective types using S-band radar data. The method of moments is employed to estimate the parameters of lognormal DSD. The modeled DSD parameters are optimized by examining the root mean square (RMS) error and the average probability ratio (APR) in estimation of the rain rate, rain attenuation, and radar reflectivity factor simultaneously. The proposed model gives maximum (close to unity) APR and minimum RMS error when compared to any other set of DSD parameters.
机译:随着使用更高频率的通信服务在热带地区迅速增长,对预测降雨引起的衰减的更精细模型的需求日益增加。在任何预测模型中,雨滴大小分布(DSD)都是主要的误差来源之一,这主要是因为其时空变化。 DSD参数是根据使用S波段雷达数据分类为层状和对流类型的地层仪数据计算得出的。矩量法用于估计对数正态DSD的参数。通过同时检查均方根(RMS)误差和平均概率比(APR)来估计降雨率,降雨衰减和雷达反射率因子,可以优化建模的DSD参数。与任何其他DSD参数集相比,该模型可提供最大(接近于单位)的APR和最小RMS误差。

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