A closed-form waveguide invariant β for a Pekeris waveguide is derived. It is based on the modal Wentzel-Kramers-Brillouin (WKB) dispersion equation and implicit differentiation, in conjunction with the concept of the "effective boundary depth," ΔH(θ), where θ is the propagation angle. First, an explicit formula for β(m,n) between mode pairs is obtained assuming an ideal waveguide of the effective waveguide depth, H+ΔH(θ), and provides an excellent agreement with the reference value for the Pekeris waveguide of depth H obtained using the normal mode program kraken. Then, a closed-form expression for a group of adjacent modes is derived: β=(H+ΔH(θ))/(H/ cos θ-ΔH(θ)), which can be approximated by β=cos θ as ΔH(θ)/H≪1, the analytical expression for an ideal waveguide.
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http://dx.doi.org/10.1121/10.0009387 | DOI Listing |
J Acoust Soc Am
July 2024
Scripps Institution of Oceanography, UC San Diego, 9500 Gilman Drive, La Jolla, California 92093, USA.
A method to determine the range and bearing of a moving broadband acoustic source, such as a surface vessel, using the coherence measured on two omni-directional, vertically separated hydrophones is demonstrated using acoustic data recorded near Alvin Canyon on the New England shelf break. To estimate the vessel's range, two theoretical approaches, a half-space model and a Pekeris waveguide model based on normal modes, establish simple relationships between the broadband signal coherence and frequency, source range, and the vertical separation of the receiver hydrophones. A brute force inversion produces a passive acoustic estimate of vessel range.
View Article and Find Full Text PDFJ Acoust Soc Am
December 2022
Naval Undersea Warfare Center, Newport, Rhode Island 02841, USA.
This paper studies resolution of matched field processing for locating, in range and depth, a broadband underwater acoustic source from data measured at a single hydrophone receiver. For the case of an ideal rigid shallow-water waveguide with a pressure-release top boundary and a rigid bottom boundary, the paper derives approximations for the main-lobe widths of the ambiguity surface. The two cases studied in this paper are (1) when coherent measurements of the pressure are available, with the transmitted source waveform precisely known, and (2) when only measurements of the received-signal pressure magnitude-squared are available, such as might occur when the transmitted signal is random and unknown.
View Article and Find Full Text PDFJASA Express Lett
January 2022
Retired, 99F Hugo Road, North Stonington, Connecticut 06359, USA
The acoustic field in an attenuating Pekeris waveguide is the limit of the field in a waveguide that is truncated at progressively larger depths. The rate of convergence is determined based on rigorous numerics using a contraction mapping in a properly formulated norm, based on Rayleigh's theorem. Given a predetermined error, the contraction mapping formulation allows the determination of the truncation depth that is needed to obtain an approximation of the field in the waveguide with the required error.
View Article and Find Full Text PDFJ Acoust Soc Am
February 2022
Scripps Institution of Oceanography, La Jolla, California 92093-0238, USA.
A closed-form waveguide invariant β for a Pekeris waveguide is derived. It is based on the modal Wentzel-Kramers-Brillouin (WKB) dispersion equation and implicit differentiation, in conjunction with the concept of the "effective boundary depth," ΔH(θ), where θ is the propagation angle. First, an explicit formula for β(m,n) between mode pairs is obtained assuming an ideal waveguide of the effective waveguide depth, H+ΔH(θ), and provides an excellent agreement with the reference value for the Pekeris waveguide of depth H obtained using the normal mode program kraken.
View Article and Find Full Text PDFJ Acoust Soc Am
December 2020
Collaborative Innovation Center for Advanced Ship and Deep-Sea Exploration, State Key Laboratory of Ocean Engineering, Shanghai Jiao Tong University, Shanghai 200240, China.
The Green's function retrieval in media with horizontal boundaries usually only considers the extraction of direct and reflected waves but ignores the virtual head waves, which have been observed experimentally from ocean ambient noise and used to invert for geometric and environmental parameters. This paper derives the extraction of virtual head waves from ocean ambient noise using a vertically spaced sensor pair in a Pekeris waveguide. Ocean ambient noise in the water column is a superposition of direct, reflected, and head waves.
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