2010
DOI: 10.1121/1.3383959
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Impact of surface gravity waves on high-frequency acoustic propagation in shallow water.

Abstract: Sea surface roughness is one of several factors that significantly influences high-frequency (1–50-kHz) acoustic wave propagation in shallow water. The evolving sea surface introduces several variability effects including Doppler shift. Data analyses from high-frequency acoustic experiments show high-correlation between time, angle, and intensity fluctuations of received signals and varying sea surface conditions. In order to assess detailed acoustic signal interactions with the sea surface, a realistic wave m… Show more

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Cited by 18 publications
(15 citation statements)
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“…Some of these techniques are the shooting, self-consistency and relaxation techniques [21][22][23][24][25]. One of the most commonly used methods for this purpose is the Petviashvili's method, in which the governing nonlinear equation is transformed into Fourier space similar to the other Fourier spectral methods using FFT routines [26][27][28][29][30][31][32][33][34][35][36][37][38][39][40]. Then, a convergence factor is used in accordance with the degree of the nonlinear term [21,22].…”
Section: Spectral Renormalization Methods For Finding the Self-locali...mentioning
confidence: 99%
“…Some of these techniques are the shooting, self-consistency and relaxation techniques [21][22][23][24][25]. One of the most commonly used methods for this purpose is the Petviashvili's method, in which the governing nonlinear equation is transformed into Fourier space similar to the other Fourier spectral methods using FFT routines [26][27][28][29][30][31][32][33][34][35][36][37][38][39][40]. Then, a convergence factor is used in accordance with the degree of the nonlinear term [21,22].…”
Section: Spectral Renormalization Methods For Finding the Self-locali...mentioning
confidence: 99%
“…The high order spectral method summarized in this section is first presented in 4 ; which models the nonlinear ocean surface waves on the surface of an ideal fluid. An implementation of this model both in 1D and 2D can be seen in 1 2 3 5 .…”
Section: Methodsmentioning
confidence: 99%
“…In SSFM schemes, the spatial derivatives are evaluated using spectral techniques. Some of the applications of the spectral techniques can be seen in [7,19,20] and more detailed discussions can be seen in [23]. In spectral techniques the spatial derivatives are calculated by making use of the orthogonal transforms.…”
Section: Chaotic Wave Fieldsmentioning
confidence: 99%