Validity criteria for the small slope approximation for backscattering of sound from rough surfaces with a power-law roughness spectrum

The small slope approximation is a commonly used model for scattering of waves from rough surfaces. Its limitations are currently unknown for a power-law roughness spectral density, used to model natural terrain and seafloor roughness. This work compares the small slope approximation to the boundary element method, a numerical solution of the Helmholtz boundary integral equations governing acoustic scattering. These comparisons were used to find the validity limits as a function of dimensionless root mean square height, kh, and root mean square slope, s, where k is the wavenumber. The two lowest terms in the small slope series were used, and both the Dirichlet and fluid-fluid boundary conditions were examined. Both kh and s are found to be important parameters for the validity of the small slope approximation. Different spectral exponents have similar maximum valid kh. The maximum s is almost constant as a function of the power law outer scale, but varies as a function of the spectral exponent. Comparisons with other scattering models are discussed, and aspects of scattering from very large roughness are explored.

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Publication Details

Journal
The Journal of the Acoustical Society of America
Published
2026-09-01
DOI
https://doi.org/10.1121/10.0046233
Primary Topic
Underwater Acoustics Research
Type
article
Field-Weighted Citation Impact
0.00

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article

Validity criteria for the small slope approximation for backscattering of sound from rough surfaces with a power-law roughness spectrum

Derek R. Olson
The Journal of the Acoustical Society of America
Underwater Acoustics Research
article

Validity criteria for the small slope approximation for backscattering of sound from rough surfaces with a power-law roughness spectrum

Derek R. Olson
article en

Abstract

The small slope approximation is a commonly used model for scattering of waves from rough surfaces. Its limitations are currently unknown for a power-law roughness spectral density, used to model natural terrain and seafloor roughness. This work compares the small slope approximation to the boundary element method, a numerical solution of the Helmholtz boundary integral equations governing acoustic scattering. These comparisons were used to find the validity limits as a function of dimensionless root mean square height, kh, and root mean square slope, s, where k is the wavenumber. The two lowest terms in the small slope series were used, and both the Dirichlet and fluid-fluid boundary conditions were examined. Both kh and s are found to be important parameters for the validity of the small slope approximation. Different spectral exponents have similar maximum valid kh. The maximum s is almost constant as a function of the power law outer scale, but varies as a function of the spectral exponent. Comparisons with other scattering models are discussed, and aspects of scattering from very large roughness are explored.

The Journal of the Acoustical Society of AmericaVol. 160(3)
Naval Postgraduate School (US)
U.S. Navy, Office of Naval Research
Life below water
Openalex Percentile: Top 13%
Underwater Acoustics Research
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