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Performance analysis of underwater vertical wireless optical communication system in the presence of weak turbulence, pointing errors and attenuation losses

机译:水下垂直无线通信系统在弱湍流、指向误差和衰减损耗下的性能分析

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摘要

In this paper, we have investigated the performance of underwater vertical wireless optical communication (UVWOC) link employing on-off key modulation in the presence of underwater turbulence, pointing errors and attenuation losses. The turbulence of the medium (assumed to be weak turbulence) has been modeled by employing the hyperbolic tangent log normal (HTLN) distribution. Temperature, pressure and salinity are parameters which can bring about variation of optical transmission characteristics with respect to depth of the ocean/sea. An in-depth study of optical transmission through vertical oceanic links requires the the underwater medium to be modeled as comprising of non-identical turbulent layers. Each of these independent and non-identical turbulence layers are modeled using the HTLN distribution function. The pointing error due to misalignment between source and detector is modeled using Rayleigh displacement pointing error. A novel closed-form expression to quantify the average bit error rate (BER) has been derived for single input single output (SISO) communication link. This expression has then been further generalized to make it applicable to the case of receive diversity schemes such as selection combining, majority logic combining and maximum ratio combining. The expression for the average BER associated with the UVWOC link for different pointing errors, different data rates and different types of ocean water has been determined. Novel closed-form expressions quantifying the outage probability and ergodic channel capacity have been derived for SISO and SC receive diversity schemes. The accuracy of all of the closed-form expressions derived in this paper have been validated using Monte-Carlo simulations.
机译:本文研究了在存在水下湍流、指向误差和衰减损耗的情况下采用开关键调制的水下垂直无线光通信(UVWOC)链路的性能。介质的湍流(假设为弱湍流)已通过采用双曲切对数正态 (HTLN) 分布进行建模。温度、压力和盐度是可以引起光传输特性相对于海洋深度变化的参数。通过垂直海洋链路对光传输的深入研究需要将水下介质建模为由不相同的湍流层组成。这些独立且不相同的湍流层中的每一个都使用 HTLN 分布函数进行建模。使用瑞利位移指向误差对源和探测器之间未对准引起的指向误差进行建模。该文推导了一种新的闭式表达式,用于量化单输入单输出(SISO)通信链路的平均误码率(BER)。然后,该表达式被进一步推广,使其适用于接收多样性方案的情况,例如选择组合、多数逻辑组合和最大比率组合。已经确定了与UVWOC链路相关的不同指向误差、不同数据速率和不同类型海水的平均误码率的表达式。已经为SISO和SC接收分集方案推导出了量化中断概率和遍历信道容量的新型闭式表达式。本文中推导的所有闭式表达式的准确性均已通过蒙特卡罗模拟进行了验证。

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