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基于观测的弯曲海洋内波中声音的建模:对短程深海声道和表面声道的研究。

Observationally constrained modeling of sound in curved ocean internal waves: examination of deep ducting and surface ducting at short range.

机构信息

Department of Applied Ocean Physics and Engineering, Woods Hole Oceanographic Institution, Woods Hole, Massachusetts 02543, USA.

出版信息

J Acoust Soc Am. 2011 Sep;130(3):1173-87. doi: 10.1121/1.3605565.

DOI:10.1121/1.3605565
PMID:21895060
Abstract

A study of 400 Hz sound focusing and ducting effects in a packet of curved nonlinear internal waves in shallow water is presented. Sound propagation roughly along the crests of the waves is simulated with a three-dimensional parabolic equation computational code, and the results are compared to measured propagation along fixed 3 and 6 km source/receiver paths. The measurements were made on the shelf of the South China Sea northeast of Tung-Sha Island. Construction of the time-varying three-dimensional sound-speed fields used in the modeling simulations was guided by environmental data collected concurrently with the acoustic data. Computed three-dimensional propagation results compare well with field observations. The simulations allow identification of time-dependent sound forward scattering and ducting processes within the curved internal gravity waves. Strong acoustic intensity enhancement was observed during passage of high-amplitude nonlinear waves over the source/receiver paths, and is replicated in the model. The waves were typical of the region (35 m vertical displacement). Two types of ducting are found in the model, which occur asynchronously. One type is three-dimensional modal trapping in deep ducts within the wave crests (shallow thermocline zones). The second type is surface ducting within the wave troughs (deep thermocline zones).

摘要

本文研究了浅水中一包弯曲非线性内波的 400 Hz 聚焦和波导效应。利用三维抛物线方程计算程序对大致沿波峰传播的声音进行了模拟,并将结果与沿固定的 3 公里和 6 公里声源/接收器路径的测量结果进行了比较。测量是在东沙岛东北的南海大陆架上进行的。在建模模拟中,时变三维声速场的构建是由与声数据同时采集的环境数据指导的。计算的三维传播结果与现场观测吻合较好。模拟允许识别弯曲内重力波内的时变声前向散射和波导过程。在源/接收器路径上经过高强度非线性波时,观察到强烈的声强增强,在模型中得到了再现。这些波是该地区的典型波(35 米垂直位移)。在模型中发现了两种类型的波导,它们是异步发生的。一种是在波峰(浅层温跃层区)内的深波导中的三维模态俘获。第二种是在波谷内的表面波导(深层温跃层区)。

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