A computer model for sound propagation around conical seamounts

Thesis (S.M.)--Massachusetts Institute of Technology, Dept. of Ocean Engineering, 2001. === Includes bibliographical references (leaves 67-69). === This paper demonstrates a technique for computing the long-range sound pressure field around a penetrable conical seamount. The pressure field is genera...

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Main Author: Eskenazi, Jérémie, 1976-
Other Authors: Arthur B. Baggeroer.
Format: Others
Language:English
Published: Massachusetts Institute of Technology 2005
Subjects:
Online Access:http://hdl.handle.net/1721.1/8778
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spelling ndltd-MIT-oai-dspace.mit.edu-1721.1-87782019-05-02T16:06:41Z A computer model for sound propagation around conical seamounts computer model for acoustic propagation around conical seamounts Eskenazi, Jérémie, 1976- Arthur B. Baggeroer. Massachusetts Institute of Technology. Dept. of Ocean Engineering. Massachusetts Institute of Technology. Dept. of Ocean Engineering. Ocean Engineering. Thesis (S.M.)--Massachusetts Institute of Technology, Dept. of Ocean Engineering, 2001. Includes bibliographical references (leaves 67-69). This paper demonstrates a technique for computing the long-range sound pressure field around a penetrable conical seamount. The pressure field is generated by a harmonic point source. The seamount is positioned in a vertically stratified ocean. It is modeled as an outgrowth of the sediment layer covering the ocean bottom. First, the seamount is decomposed into superposed rings of diameters increasing with the depth. Thus the problem reduces to a cylindrically layered system. Then, the method of normal modes is used to compute the sound pressure field in each layer. In order to maintain numerical stability, the Direct Global Matrix approach is used. The radial eigenfunctions are expressed as functions of normalized Hankel and Bessel functions, and the linear system that arise is organized in an unconditionally stable matrix. The results show a perturbation zone behind the seamount. It is bounded by two lines going from the source and tangent to the ring that is at the depth of the source. The values of the sound pressure inside the perturbation zone can be higher or lower than the values outside of it, according to the dimensions of the seamount. by Jérémie Eskenazi. S.M. 2005-08-23T15:15:19Z 2005-08-23T15:15:19Z 2001 2001 Thesis http://hdl.handle.net/1721.1/8778 48166506 eng M.I.T. theses are protected by copyright. They may be viewed from this source for any purpose, but reproduction or distribution in any format is prohibited without written permission. See provided URL for inquiries about permission. http://dspace.mit.edu/handle/1721.1/7582 69 leaves 4464387 bytes 4464143 bytes application/pdf application/pdf application/pdf Massachusetts Institute of Technology
collection NDLTD
language English
format Others
sources NDLTD
topic Ocean Engineering.
spellingShingle Ocean Engineering.
Eskenazi, Jérémie, 1976-
A computer model for sound propagation around conical seamounts
description Thesis (S.M.)--Massachusetts Institute of Technology, Dept. of Ocean Engineering, 2001. === Includes bibliographical references (leaves 67-69). === This paper demonstrates a technique for computing the long-range sound pressure field around a penetrable conical seamount. The pressure field is generated by a harmonic point source. The seamount is positioned in a vertically stratified ocean. It is modeled as an outgrowth of the sediment layer covering the ocean bottom. First, the seamount is decomposed into superposed rings of diameters increasing with the depth. Thus the problem reduces to a cylindrically layered system. Then, the method of normal modes is used to compute the sound pressure field in each layer. In order to maintain numerical stability, the Direct Global Matrix approach is used. The radial eigenfunctions are expressed as functions of normalized Hankel and Bessel functions, and the linear system that arise is organized in an unconditionally stable matrix. The results show a perturbation zone behind the seamount. It is bounded by two lines going from the source and tangent to the ring that is at the depth of the source. The values of the sound pressure inside the perturbation zone can be higher or lower than the values outside of it, according to the dimensions of the seamount. === by Jérémie Eskenazi. === S.M.
author2 Arthur B. Baggeroer.
author_facet Arthur B. Baggeroer.
Eskenazi, Jérémie, 1976-
author Eskenazi, Jérémie, 1976-
author_sort Eskenazi, Jérémie, 1976-
title A computer model for sound propagation around conical seamounts
title_short A computer model for sound propagation around conical seamounts
title_full A computer model for sound propagation around conical seamounts
title_fullStr A computer model for sound propagation around conical seamounts
title_full_unstemmed A computer model for sound propagation around conical seamounts
title_sort computer model for sound propagation around conical seamounts
publisher Massachusetts Institute of Technology
publishDate 2005
url http://hdl.handle.net/1721.1/8778
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