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Alphasat Aldo Paraboni propagation experiment in Graz - frequency scaling analysis

机译:Alphasat Aldo Paraboni在格拉茨的传播实验-频率缩放分析

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In order to study propagation effects for future satellite communication frequencies, the Alphasat Aldo Paraboni payload includes two beacon transmitters at Ka-band (19.701 GHz) and Q-band (39.402 GHz). Among all atmospheric effects, rain has the biggest impact on signal transmission. Often a single statistical relationship (derived from climatic parameters) between rain rate and specific attenuation is used, but it is well known that the variability of the drop size distribution (DSD) for a given rain rate is considerably large and affects the specific attenuation. Frequency scaling is often applied to determine the instantaneous attenuation at the uplink (higher frequency) from a measured attenuation at the downlink (lower frequency). This paper reports on the propagation and disdrometer measurements carried out in Graz (Austria) during 2014. The instantaneous frequency scaling factor obtained from DSD data is analyzed and the instantaneous frequency scaling ITU-R model is compared against beacon measurements.
机译:为了研究未来卫星通信频率的传播影响,Alphasat Aldo Paraboni有效载荷包括两个在Ka频段(19.701 GHz)和Q频段(39.402 GHz)的信标发射机。在所有大气影响中,雨水对信号传输的影响最大。通常使用降雨率和特定衰减之间的单个统计关系(从气候参数得出),但是众所周知,对于给定的降雨率,液滴尺寸分布(DSD)的变化很大,并且会影响特定衰减。通常使用频率缩放来从测量的下行链路(低频)衰减确定上行链路(高频)的瞬时衰减。本文报告了2014年在格拉茨(奥地利)进行的传播和测距仪测量。分析了从DSD数据获得的瞬时频率缩放因子,并将瞬时频率缩放ITU-R模型与信标测量进行了比较。

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