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Three-Dimensional Inversion Techniqu...

Roa, Camilo Carlos.

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Three-Dimensional Inversion Technique in Ocean Acoustics Using the Parabolic Equation Method.

Record Type:	Electronic resources : Monograph/item
Title/Author:	Three-Dimensional Inversion Technique in Ocean Acoustics Using the Parabolic Equation Method./
Author:	Roa, Camilo Carlos.
Published:	Ann Arbor : ProQuest Dissertations & Theses, : 2017,
Description:	193 p.
Notes:	Source: Dissertation Abstracts International, Volume: 78-10(E), Section: B.
Contained By:	Dissertation Abstracts International78-10B(E).
Subject:	Ocean engineering. -
Online resource:	http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=10610495
ISBN:	9781369849271

Three-Dimensional Inversion Technique in Ocean Acoustics Using the Parabolic Equation Method.
Roa, Camilo Carlos.

Three-Dimensional Inversion Technique in Ocean Acoustics Using the Parabolic Equation Method. - Ann Arbor : ProQuest Dissertations & Theses, 2017 - 193 p.

Source: Dissertation Abstracts International, Volume: 78-10(E), Section: B.

Thesis (Ph.D.)--Florida Atlantic University, 2017.

A three-dimensional parabolic equation (PE) and perturbation approach is used to invert for the depth- and range-dependent geoacoustic characteristics of the seabed. The model assumes that the sound speed profile is the superposition of a known range-independent profile and an unknown depth- and range-dependent perturbation. Using a Green's function approach, the total measured pressure field in the water column is decomposed into a background field, which is due to the range-independent profile, and a scattered field, which is due to the range-dependent perturbation. When the Born approximation is applied to the resulting integral equation, it can be solved for the range-dependent profile using linear inverse theory. Although the method is focused on inverting for the sound speed profile in the bottom, it can also invert for the sound speed profile in the water column. For simplicity, the sound speed profile in the water column was assumed to be known with a margin of error of +/- 5 m/s. The range-dependent perturbation is added to the index of refraction squared n2(r), rather than the sound speed profile c(ro). The method is implemented in both Cartesian (x,y,z) and cylindrical (r,q,z) coordinates with the forward propagation of the field in x and r, respectively. Synthetic data are used to demonstrate the validity of the method [1].

ISBN: 9781369849271Subjects--Topical Terms:

660731
Ocean engineering.

Three-Dimensional Inversion Technique in Ocean Acoustics Using the Parabolic Equation Method.
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100 1 $a Roa, Camilo Carlos. $3 3427189
245 1 0 $a Three-Dimensional Inversion Technique in Ocean Acoustics Using the Parabolic Equation Method.
260 1 $a Ann Arbor : $b ProQuest Dissertations & Theses, $c 2017
300 $a 193 p.
500 $a Source: Dissertation Abstracts International, Volume: 78-10(E), Section: B.
500 $a Adviser: George V. Frisk.
502 $a Thesis (Ph.D.)--Florida Atlantic University, 2017.
520 $a A three-dimensional parabolic equation (PE) and perturbation approach is used to invert for the depth- and range-dependent geoacoustic characteristics of the seabed. The model assumes that the sound speed profile is the superposition of a known range-independent profile and an unknown depth- and range-dependent perturbation. Using a Green's function approach, the total measured pressure field in the water column is decomposed into a background field, which is due to the range-independent profile, and a scattered field, which is due to the range-dependent perturbation. When the Born approximation is applied to the resulting integral equation, it can be solved for the range-dependent profile using linear inverse theory. Although the method is focused on inverting for the sound speed profile in the bottom, it can also invert for the sound speed profile in the water column. For simplicity, the sound speed profile in the water column was assumed to be known with a margin of error of +/- 5 m/s. The range-dependent perturbation is added to the index of refraction squared n2(r), rather than the sound speed profile c(ro). The method is implemented in both Cartesian (x,y,z) and cylindrical (r,q,z) coordinates with the forward propagation of the field in x and r, respectively. Synthetic data are used to demonstrate the validity of the method [1].
520 $a Two inversion methods were combined, a Monte Carlo like algorithm, responsible for a starting approximation of the sound speed profile, and a steepest descent method, that fine-tuned the results. In simulations, the inversion algorithm is capable of inverting for the sound speed profile of a flat bottom. It was tested, for three different frequencies (50 Hz, 75 Hz, and 100 Hz), in a Pekeris waveguide, a range-independent layered medium, and a range-dependent medium, with errors in the inverted sound speed profile of less than 3%.
590 $a School code: 0119.
650 4 $a Ocean engineering. $3 660731
650 4 $a Physical oceanography. $3 3168433
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710 2 $a Florida Atlantic University. $b Ocean and Mechanical Engineering. $3 3175699
773 0 $t Dissertation Abstracts International $g 78-10B(E).
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791 $a Ph.D.
792 $a 2017
793 $a English
856 4 0 $u http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=10610495