首页> 外文期刊>Telecommunications and Radio Engineering >TROPOSPHERIC SCINTILLATION EFFECTS ON SATELLITE LINKS FROM X-BAND TO Q-BAND OVER NIGERIAN CLIMATIC ZONES USING KARASAWA AND ITU-R MODELS
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TROPOSPHERIC SCINTILLATION EFFECTS ON SATELLITE LINKS FROM X-BAND TO Q-BAND OVER NIGERIAN CLIMATIC ZONES USING KARASAWA AND ITU-R MODELS

机译:使用Karasawa和ITU-R型号,从X波段到Q频段的卫星链路对卫星链接的闪烁闪烁效应

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The tropospheric scintillation of satellite communication signals has continued to draw the attention of radio engineers. The effect and prevalent paucity of Earth-space tropospheric scintillation data in Africa are remarkable. The parameters of NigComSat-1R and Eutelsat-36B satellites were used for this modeling from X- to Q-band during the West African monsoon (WAM). The low error rates of Karasawa and ITU-R models reported for the tropical climates made them appropriate for this study. In situ data from the Tropospheric Data Acquisition Network stations spanning three climatic regions in Nigeria, namely Tropical Monsoon, Geo. 6.5° N, 3.5° E; Tropical Savanna, Geo. 8.99° N, 7.38° E; and the Sahel, Geo. 9.35° N, 12.5° E. The scintillation variability is lowest in the tropical monsoon climate and highest in the Sahel climate using both models. However, the ITU-R model recorded higher scintillation fade depths (SFDs) of 37.19 dB, 2.91 dB, and 2.52 dB, for low elevation, NigComSat-1R and Eutelsat-36B satellites respectively, over the tropical monsoon climatic zone, than Karasawa model, which recorded SFDs of 34.07 dB, 1.31 dB, and 1.09 dB for the respective satellites. The observed scintillation intensity increased with increasing carrier frequency, low elevation angle and small receiving antenna. High variability of the scintillation intensity characterizes the onset of WAM and post-monsoon months.
机译:卫星通信信号的对流层闪烁已经继续引起无线电工程师的注意。非洲地球空间对流层闪烁数据的效果和普遍缺乏缺乏卓越。 Nigcomsat-1R和Eutelsat-36B卫星的参数用于西非季风(WAM)期间从X到Q波段的这种建模。为热带气候报告的Karasawa和ITU-R模型的低错误率使其适合这项研究。原位数据来自跨国跨越三个气候区域的对流层数据采集网络站,即热带季风,地理。 6.5°N,3.5°E;热带大草原,地理。 8.99°N,7.38°E;和萨赫尔,地理。 9.35°N,12.5°E。闪烁变异性在热带季风气候下最低,使用两种型号的萨赫兰气候中最高。然而,ITU-R模型在热带季风气候区分别记录了37.19dB,2.91dB,2.52 dB的37.19 dB,2.91 dB和2.52 dB的闪烁淡化深度(SFD),而不是Karasawa模型,其录制了34.07 dB,1.31 dB,1.09 dB的SFD,适用于各种卫星。观察到的闪烁强度随着载波频率,低仰角和小接收天线的增加而增加。闪烁强度的高可变性表征WAM和季风月后的发作。

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