High frequency rough surface parabolic equation modeling for underwater acoustic communications

Allan P. Rosenberg, D. Chizhik, Qinqing Zhang
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引用次数: 6

Abstract

In this paper, we propose to develop an effective and efficient computational modeling technique to characterize the statistical properties that govern the performance and capacity of an underwater acoustic communication link. Specifically, we consider the challenging shallow water environment with a moving rough sea surface as the primary source of temporal variations. We incorporate a realistic sea surface for wind driven waves generated by the surface spectrum. We use meteorological and oceanic data measured by National Data Buoy Center (NDBC) buoy 44014 (36.611N 74.836W) and model estimates of downward radiation fluxes at its location to produce a time series, covering all of 2004 with 3 hr spacing, of the input parameters needed by the analytical spectral model. For one particular set of parameters, typical of March, we generate sea surface realizations and study their effect on acoustic propagation. We extend a parabolic equation (PE) model to compute the propagation of a high frequency, wide-band acoustic transmission with a time-varying sea surface. We provide numerical results of received signal power as a function of range and depth. Our modeling approach has both physical applicability and computation feasibility to generate channel impulse responses useful for adaptive underwater communications.
水声通信高频粗糙面抛物方程建模
在本文中,我们建议开发一种有效和高效的计算建模技术来表征控制水声通信链路性能和容量的统计特性。具体来说,我们认为具有挑战性的浅水环境与移动的粗糙海面是时间变化的主要来源。我们结合了一个真实的海面,由海面光谱产生的风驱动波。利用美国国家数据浮标中心(NDBC) 44014号浮标(36.611N 74.836W)测得的气象和海洋资料以及该浮标所在位置的向下辐射通量模型估算值,得到了分析光谱模型所需输入参数的时间序列,该序列覆盖2004年全年,间隔为3 h。对于一个特定的参数集,典型的三月,我们生成海面实现并研究它们对声波传播的影响。我们扩展了抛物方程(PE)模型来计算具有时变海面的高频宽带声传输的传播。我们提供了接收信号功率作为距离和深度函数的数值结果。我们的建模方法具有物理适用性和计算可行性,可以生成用于自适应水下通信的信道脉冲响应。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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