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Updated: Feb 17, 2026

Scattering And Absorption of Light in Planetary Regoliths
Published on: July 1, 2019
A time-domain model for seafloor scattering
1Applied Physics Laboratory, University of Washington, Seattle, Washington 98105, USA.
Abstract:
Bottom scattering is important for a number of underwater applications: it is a source of noise in target detection and a source of information for sediment classification and geoacoustic inversion. While current models can predict the effective interface scattering strength for layered sediments, these models cannot directly compute the ensemble averaged mean-square pressure. A model for bottom scattering due to a point source is introduced which provides a full-wave solution for mean-square scattered pressure as a function of time under first-order perturbation theory. Examples of backscatter time series from various types of seafloors will be shown, and the advantages and limitations of this model will be discussed.
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