Perturbative inversion of geoacoustic parameters in a shallow water environment

In many strategic shallow water areas the geoacoustic properties of the sub-bottom are largely unknown. In this thesis it is demonstrated that inverse theory and measured data from a single hydrophone can be used to accurately deduce the geoacoustic properties of the sub-bottom, even when the initia...

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Main Author: Null, James Mark.
Other Authors: Bourke, Robert H.
Language:en_US
Published: Monterey, California. Naval Postgraduate School 2012
Online Access:http://hdl.handle.net/10945/7545
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spelling ndltd-nps.edu-oai-calhoun.nps.edu-10945-75452015-07-02T16:03:26Z Perturbative inversion of geoacoustic parameters in a shallow water environment Null, James Mark. Bourke, Robert H. Wilson, James H. Meteorology and Physical Oceanography In many strategic shallow water areas the geoacoustic properties of the sub-bottom are largely unknown. In this thesis it is demonstrated that inverse theory and measured data from a single hydrophone can be used to accurately deduce the geoacoustic properties of the sub-bottom, even when the initial background geoacoustic model is a highly inaccurate guess. Since propagation in shallow water is very sensitive to the geoacoustic properties of the sub-bottom, the inverse technique developed in this thesis presents the Navy with a vitally important, practical, and inexpensive means to improve sonar performance prediction in a potentially hostile environment. To provide ground truth for the inverse technique, measured data collected during Project GEMINI were compared to the inverse solutions. Detailed, site-specific geoacoustic models were developed for two array locations and the Finite Element Parabolic Equation (FEPE) model was used to estimate transmission loss (TL). The model estimates from FEPE compared well with the measured data and the detailed geoacoustic models were considered as ground truth. To test the efficacy of the technique, initial background geoacoustic models were constructed assuming no a priori information of the bottom. The resultant inverse solution was used to predict the geoacoustic properties at each of the sites. The final results were in excellent agreement with the measured data and the resulting inverse technique TL estimates were as good or better than the Th estimates obtained from the detailed, site-specific geoacoustic models. (AN) 2012-07-31T19:54:17Z 2012-07-31T19:54:17Z 1995-03 Thesis http://hdl.handle.net/10945/7545 en_US This publication is a work of the U.S. Government as defined in Title 17, United States Code, Section 101. As such, it is in the public domain, and under the provisions of Title 17, United States Code, Section 105, it may not be copyrighted. Monterey, California. Naval Postgraduate School
collection NDLTD
language en_US
sources NDLTD
description In many strategic shallow water areas the geoacoustic properties of the sub-bottom are largely unknown. In this thesis it is demonstrated that inverse theory and measured data from a single hydrophone can be used to accurately deduce the geoacoustic properties of the sub-bottom, even when the initial background geoacoustic model is a highly inaccurate guess. Since propagation in shallow water is very sensitive to the geoacoustic properties of the sub-bottom, the inverse technique developed in this thesis presents the Navy with a vitally important, practical, and inexpensive means to improve sonar performance prediction in a potentially hostile environment. To provide ground truth for the inverse technique, measured data collected during Project GEMINI were compared to the inverse solutions. Detailed, site-specific geoacoustic models were developed for two array locations and the Finite Element Parabolic Equation (FEPE) model was used to estimate transmission loss (TL). The model estimates from FEPE compared well with the measured data and the detailed geoacoustic models were considered as ground truth. To test the efficacy of the technique, initial background geoacoustic models were constructed assuming no a priori information of the bottom. The resultant inverse solution was used to predict the geoacoustic properties at each of the sites. The final results were in excellent agreement with the measured data and the resulting inverse technique TL estimates were as good or better than the Th estimates obtained from the detailed, site-specific geoacoustic models. (AN)
author2 Bourke, Robert H.
author_facet Bourke, Robert H.
Null, James Mark.
author Null, James Mark.
spellingShingle Null, James Mark.
Perturbative inversion of geoacoustic parameters in a shallow water environment
author_sort Null, James Mark.
title Perturbative inversion of geoacoustic parameters in a shallow water environment
title_short Perturbative inversion of geoacoustic parameters in a shallow water environment
title_full Perturbative inversion of geoacoustic parameters in a shallow water environment
title_fullStr Perturbative inversion of geoacoustic parameters in a shallow water environment
title_full_unstemmed Perturbative inversion of geoacoustic parameters in a shallow water environment
title_sort perturbative inversion of geoacoustic parameters in a shallow water environment
publisher Monterey, California. Naval Postgraduate School
publishDate 2012
url http://hdl.handle.net/10945/7545
work_keys_str_mv AT nulljamesmark perturbativeinversionofgeoacousticparametersinashallowwaterenvironment
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