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Effects of meteorological parameters and the averaging period on the intensity of tropospheric scintillation

机译:气象参数和平均周期对对流层闪烁强度的影响

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摘要

The saturation of C-band and the ever-increasing demand for new services that require greater bandwidth has pushed to the exploitation of higher frequencies. The higher frequencies offer various advantages such as, increased bandwidth, smaller antennas, and smaller satellite footprint that give higher EIRP and permit frequency reuse. The main obstacle however is that they are subject to stronger propagation degradation. The small size antennas employed in VSAT and USAT systems significantly reduces the cost of Earth stations terminals and also eliminate tracking requirements, they nevertheless lose the mitigating effect of aperture averaging, and hence experience stronger scintillation. Scintillations are rapid fluctuations in amplitude and phase of the received signal arising from fluctuations in the atmospheric refractive index due to turbulence. Amplitude scintillation occurring in the troposphere increases with signal frequency and depends on a number of other link and meteorological parameters. In this paper the attention is focused on investigating the characteristics of tropospheric scintillation at 18.7, 39.6 and 49.5 GHz using propagation data from the ITALSAT F1 and ITALSAT F2 satellites.
机译:C波段的饱和以及对需要更大带宽的新服务的需求不断增长,这促使人们开发更高的频率。较高的频率具有各种优势,例如带宽增加,天线更小以及卫星覆盖区更小,这些都带来了更高的EIRP并允许频率复用。然而,主要的障碍是它们遭受更强的传播退化。 VSAT和USAT系统中使用的小尺寸天线显着降低了地球站终端的成本,并且消除了跟踪要求,但它们却失去了孔径平均的缓解作用,因此经历了更强的闪烁。闪烁是由于湍流引起的大气折射率波动而引起的接收信号幅度和相位的快速波动。对流层中发生的幅度闪烁随信号频率的增加而增加,并取决于许多其他链接和气象参数。在本文中,注意力集中在利用来自ITALSAT F1和ITALSAT F2卫星的传播数据研究18.7、39.6和49.5 GHz对流层闪烁的特性。

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