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A Study on Time Variation of Rain Attenuation Characteristics for the Kind of Rain Fronts in Ka Band Satellite Communications

机译:Ka波段卫星通信中不同类型雨锋的雨衰特性时变研究

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This study presents detailed attenuation characteristics of the Ka-band satellite signal levels observed at 1 sec interval at Osaka Electro-Communication University in Neyagawa, Osaka, from 1997 to 2007. Long-term statistics of the duration time and the fade slope are in fairly good agreement with the ITU-R predictions. In more detail, however, the cumulative probabilities of the duration time become comparatively higher in the typhoon and stationary front events as the duration time increases, while the distribution of the fade slope becomes wider in the cold front events for any threshold levels. These characteristics should be considered for better statistical predictions in Japan. Spectral analysis of the attenuation fluctuation reveals that the spectral components of the rain attenuation are confined in a frequency range of less than 0.1 Hz, i.e., in a time scale of more than 10 sec. According to the rain types, however, there seems to be no clear difference in the slope of each spectral density, indicating similar spectral components for any rain types. This suggests that the difference in the amplitude should be a main cause of the difference in the fade slope statistics for the rain types.
机译:这项研究提供了1997年至2007年在大阪市寝屋川市大阪电Osaka通信大学以1秒间隔观察到的Ka波段卫星信号电平的详细衰减特性。持续时间和衰落斜率的长期统计数据相当合理与ITU-R的预测非常吻合。然而,更详细地讲,随着持续时间的增加,在台风和静止锋面事件中持续时间的累积概率变得相对较高,而对于任何阈值水平,在冷锋事件中衰落斜率的分布变得更宽。为了更好地进行日本的统计预测,应考虑这些特征。衰减波动的频谱分析表明,降雨衰减的频谱分量被限制在小于0.1 Hz的频率范围内,即在大于10秒的时间范围内。但是,根据雨水类型,每个光谱密度的斜率似乎没有明显差异,这表明任何雨水类型的光谱成分相似。这表明幅度的差异应该是导致降雨类型的衰落斜率统计差异的主要原因。

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