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Correlation between attenuation of 20 GHz satellite communication link and Liquid Water Content in the atmosphere

机译:20 GHz卫星通信链路衰减与大气中液体含水量的相关性

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The effect of Liquid Water Content, i.e. the mass of the water per volume unit of the atmosphere, on the attenuation of a 20 GHz communication link between a ground antenna and communication satellite is tackled in this paper. The wavelength of 20 GHz electromagnetic radiation is comparable to the droplet size, consequently the scattering plays an important role in the attenuation. To better understand this phenomenon a correlation between measured LWC and attenuation is analysed. The LWC is usually estimated from the pluviograph rain rate measurements that captures only spatially localized and ground level information about the LWC. In this paper the LWC is extracted also from the reflectivity measurements provided by a 5.6 GHz weather radar situated in Lisca, Slovenia. The radar measures reflectivity in 3D and therefore a precise spatial dependency of LWC along the communication link is considered. The attenuation is measured with an in-house receiver Ljubljana Station SatProSi 1 that communicates with a geostationary communication satellite ASTRA 3B on the 20 GHz band.
机译:液体含水量的影响,即气氛的每体积单位的水的质量,在本文中地处理了地面天线和通信卫星之间的20 GHz通信连接的衰减。 20GHz电磁辐射的波长与液滴尺寸相当,因此散射在衰减中起重要作用。为了更好地理解这种现象,分析了测量的LWC与衰减之间的相关性。 LWC通常从PLuviograph雨速率测量估计,该测量仅捕获有关LWC的空间局部和地面信息。在本文中,LWC也来自由5.6 GHz天气雷达提供的反射率测量,位于斯堪塞斯卡的5.6 GHz天气雷达。雷达测量3D中的反射率,因此考虑了LWC沿通信链路的精确空间依赖性。衰减用内部接收器Ljubljana Station SatProsi 1测量,它与20GHz频段上的地球静止通信卫星ASTRA 3B通信。

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