一个有效的低掠射反射系数用于模拟随机粗糙地形上的地波传播

D. Liao, K. Sarabandi
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引用次数: 1

摘要

对于在崎岖地形上的传播,地面的物理统计特性对传播信号的统计有直接的影响。当发射器和接收器靠近时,来自发射天线的视距(LOS)空间波(当它存在时)为接收到的总信号提供了主要贡献,因为来自底层粗糙表面的相干反射被随机散射效应所减少。然而,在长距离上,当传播路径接近放牧条件时,根据瑞利准则,表面再次出现电光滑,直接和地面散射信号之间重新建立相干抵消。这些定性观察结果与之前的研究[1,2]中提出的数值模拟结果一致;具体而言,如[1]所示,对于固定的发射端和接收端位置,远场传播损耗如预期的那样随着表面均方根高度的增加而增加,但也与两点表面相关长度有相当大的依赖性。此外,在放牧传播中,不再适合用位于原始表面物理平均高度的光滑表面完全替换粗糙表面来计算相干信号统计量,因为现在有效高度是均方根高度和相关长度的函数。虽然[1,2]中规定的数值模型已被证明是处理近地通道的有效模拟器,但在分析公式中定量捕获上述观测结果也很方便,这些观测结果在现有文献中没有得到充分的处理和解释。
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An effective low-grazing reflection coefficient for modeling groundwave propagation over randomly rough terrain
For propagation over a rough terrain, the physical statistical properties of the ground surface have a direct impact on the statistics of the propagating signal. When the transmitter and receiver are close, the LOS (line-of-sight) space wave from the transmitting antenna, when it exists, provides the primary contribution to the total received signal, as the coherent reflection from the underlying rough surface is reduced by the random scattering effects. However, over a long distance, as the propagation path approaches the grazing condition, in accordance with the Rayleigh criterion, the surface appears electrically smooth again and coherent cancellation between the direct and ground scattered signals is re-established. These qualitative observations are consistent with numerical simulation results presented in previous works [1, 2]; specifically, as it has been shown in [1], for fixed transmitter and receiver locations, the far field propagation loss increases with the surface rms height as expected but also shows considerable dependence on the two-point surface correlation length. Furthermore, at grazing propagation, it is no longer proper to calculate coherent signal statistics by a complete replacement of the rough surface with a smooth surface positioned at the original surface's physical mean height, for now the effective height is a function of both rms height and correlation length. Although numerical models such as those prescribed in [1, 2] have proven to be efficient simulators in dealing with the near-ground channel, it is also convenient to quantitatively capture the aforementioned observations—which have not been sufficiently addressed and explained in existing literature—in analytical formulations.
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