PHASE FLUCTUATIONS OF THE SOUND FIELD DUE TO INTERNAL WAVES IN SHALLOW WATER

Distortion of the phase front of the sound field from the point source in shallow water in presence of intense internal waves (IW) is considered. In absence of IW phase front has cylindrical shape with axis passing through the source perpendicular to the horizontal plane. One of the main peculiariti...

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Main Authors: B. G. Katsnelson, A. V. Tshoidze
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Published: 2007
Subjects:
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.492.8704
http://www.sea-acustica.es/WEB_ICA_07/fchrs/papers/unw-04-010.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.492.8704 2023-05-15T15:39:06+02:00 PHASE FLUCTUATIONS OF THE SOUND FIELD DUE TO INTERNAL WAVES IN SHALLOW WATER B. G. Katsnelson A. V. Tshoidze The Pennsylvania State University CiteSeerX Archives 2007 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.492.8704 http://www.sea-acustica.es/WEB_ICA_07/fchrs/papers/unw-04-010.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.492.8704 http://www.sea-acustica.es/WEB_ICA_07/fchrs/papers/unw-04-010.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.sea-acustica.es/WEB_ICA_07/fchrs/papers/unw-04-010.pdf text 2007 ftciteseerx 2016-08-14T00:05:37Z Distortion of the phase front of the sound field from the point source in shallow water in presence of intense internal waves (IW) is considered. In absence of IW phase front has cylindrical shape with axis passing through the source perpendicular to the horizontal plane. One of the main peculiarities of distortion in presence of IW is frequency and modal dependencies of characteristics of this distortion. Fluctuations of the phase front is considered within the framework of theory “vertical modes and horizontal rays ” or PE in horizontal plane. It is shown that mentioned fluctuations can be measured using horizontal line array together with modes filtering. Theoretical estimations and numerical modeling is carried out for conditions of Mid Atlantic bight and Barents sea. It is known that intense IW cause significant fluctuations of the sound field in shelf zone of the Ocean. It is shown in [1,2] that significant fluctuations of the sound intensity take place if acoustic track is approximately parallel to wave front of IW due to horizontal refraction. Remark that fluctuations of sound phase (or in ray language fluctuations of direction of propagation in horizontal place) also are of great interest. Practically they can be measured using horizontal line array (HLA) simultaneously with modes filtering. Let’s consider sound propagation in 3D shallow water waveguide in presence IW (Fig.1). Water layer is restricted by the surface (X,Y), and plane Hz = , where Z-axis is directed downward. In water layer we have density distribution)(zρ and sound speed profile),,()(),, ( 0 zyxczczyxc δ+ = where some unperturbed sound speed profile and)(0 zc),, ( zyxcδ perturbation due to IW. Text Barents Sea Unknown Barents Sea
institution Open Polar
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op_collection_id ftciteseerx
language English
description Distortion of the phase front of the sound field from the point source in shallow water in presence of intense internal waves (IW) is considered. In absence of IW phase front has cylindrical shape with axis passing through the source perpendicular to the horizontal plane. One of the main peculiarities of distortion in presence of IW is frequency and modal dependencies of characteristics of this distortion. Fluctuations of the phase front is considered within the framework of theory “vertical modes and horizontal rays ” or PE in horizontal plane. It is shown that mentioned fluctuations can be measured using horizontal line array together with modes filtering. Theoretical estimations and numerical modeling is carried out for conditions of Mid Atlantic bight and Barents sea. It is known that intense IW cause significant fluctuations of the sound field in shelf zone of the Ocean. It is shown in [1,2] that significant fluctuations of the sound intensity take place if acoustic track is approximately parallel to wave front of IW due to horizontal refraction. Remark that fluctuations of sound phase (or in ray language fluctuations of direction of propagation in horizontal place) also are of great interest. Practically they can be measured using horizontal line array (HLA) simultaneously with modes filtering. Let’s consider sound propagation in 3D shallow water waveguide in presence IW (Fig.1). Water layer is restricted by the surface (X,Y), and plane Hz = , where Z-axis is directed downward. In water layer we have density distribution)(zρ and sound speed profile),,()(),, ( 0 zyxczczyxc δ+ = where some unperturbed sound speed profile and)(0 zc),, ( zyxcδ perturbation due to IW.
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author B. G. Katsnelson
A. V. Tshoidze
spellingShingle B. G. Katsnelson
A. V. Tshoidze
PHASE FLUCTUATIONS OF THE SOUND FIELD DUE TO INTERNAL WAVES IN SHALLOW WATER
author_facet B. G. Katsnelson
A. V. Tshoidze
author_sort B. G. Katsnelson
title PHASE FLUCTUATIONS OF THE SOUND FIELD DUE TO INTERNAL WAVES IN SHALLOW WATER
title_short PHASE FLUCTUATIONS OF THE SOUND FIELD DUE TO INTERNAL WAVES IN SHALLOW WATER
title_full PHASE FLUCTUATIONS OF THE SOUND FIELD DUE TO INTERNAL WAVES IN SHALLOW WATER
title_fullStr PHASE FLUCTUATIONS OF THE SOUND FIELD DUE TO INTERNAL WAVES IN SHALLOW WATER
title_full_unstemmed PHASE FLUCTUATIONS OF THE SOUND FIELD DUE TO INTERNAL WAVES IN SHALLOW WATER
title_sort phase fluctuations of the sound field due to internal waves in shallow water
publishDate 2007
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.492.8704
http://www.sea-acustica.es/WEB_ICA_07/fchrs/papers/unw-04-010.pdf
geographic Barents Sea
geographic_facet Barents Sea
genre Barents Sea
genre_facet Barents Sea
op_source http://www.sea-acustica.es/WEB_ICA_07/fchrs/papers/unw-04-010.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.492.8704
http://www.sea-acustica.es/WEB_ICA_07/fchrs/papers/unw-04-010.pdf
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
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