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Prediction of data stream parameters in atmospheric turbulent wireless communication links

机译:大气湍流无线通信链路中数据流参数的预测

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摘要

A unified approach for calculation of information data stream parameters in the atmospheric optical communication channel is presented based on irradiance fluctuations of optical wave propagation through turbulence and on a generalized Ricean K-parameter distribution. The effects of turbulence are described via the well-known Kolmogorov scheme of turbulent structure relaxation in terms of stochastic scintillation theory described by the gamma-gamma distribution along with measurements of the values of the refractive index structure parameter, C_(n)~(2). The relation between the Ricean parameter K and the signal scintillation parameter (sigma)_(I)~(2) is considered to develop a unified description of the corresponding probability density function (pdf) of signal fading within an atmospheric wireless communication link. Through the corresponding pdf and parameter K, signal data stream parameters such as the signal-to-noise ratio (SNR), bit error rate (BER), and capacity of the optical atmospheric channel (C) are estimated. Such an approach permits the reliable prediction of the effects of fading caused by different levels of turbulence and agrees with experimental data observed at different atmospheric levels, at the heights of both 100-200 m and above 1-2 km. It is shown that at heights of 100-200 m, effects of fading, caused by turbulence, occur much more frequently than those at the heights of 1-2 km. Data stream parameters such as channel capacity, SNR, and spectral efficiency become stronger at higher altitudes, while at the same time the BER becomes relatively negligible.
机译:提出了一种基于湍流传播的光波辐照度波动和广义Ricean K参数分布的统一方法,用于计算大气光通信信道中信息数据流参数。通过由伽玛-伽玛分布描述的随机闪烁理论以及对折射率结构参数C_(n)〜(2)的测量,通过众所周知的湍流结构弛豫的Kolmogorov方案描述了湍流的影响)。赖斯参数K和信号闪烁参数σ_(I)〜(2)之间的关系被认为是建立大气无线通信链路中信号衰落的相应概率密度函数(pdf)的统一描述。通过相应的pdf和参数K,可以估算出信号数据流参数,例如信噪比(SNR),误码率(BER)和光学大气通道(C)的容量。这种方法可以可靠地预测由不同湍流水平引起的衰落效应,并且与在不同大气水平,100-200 m和1-2 km以上的高度观察到的实验数据一致。结果表明,在100-200 m的高度上,由湍流引起的衰落效应比在1-2 km的高度上更为频繁地发生。数据流参数(例如信道容量,SNR和频谱效率)在更高的海拔高度变得更强,而BER则相对可以忽略不计。

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