Acoustic Observation of the Time Dependence of the Roughness of Sandy Seafloors

A statistical model for the time evolution of seafloor roughness due to biological activity is applied to photographic and acoustic data. In this model, the function describing small scale seafloor topography obeys a time-evolution equation with a random forcing term that creates roughness and a dif...

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Veröffentlicht in:IEEE journal of oceanic engineering 2009-10, Vol.34 (4), p.407-422
Hauptverfasser: Jackson, D.R., Richardson, M.D., Williams, K.L., Lyons, A.P., Jones, C.D., Briggs, K.B., Dajun Tang
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container_end_page 422
container_issue 4
container_start_page 407
container_title IEEE journal of oceanic engineering
container_volume 34
creator Jackson, D.R.
Richardson, M.D.
Williams, K.L.
Lyons, A.P.
Jones, C.D.
Briggs, K.B.
Dajun Tang
description A statistical model for the time evolution of seafloor roughness due to biological activity is applied to photographic and acoustic data. In this model, the function describing small scale seafloor topography obeys a time-evolution equation with a random forcing term that creates roughness and a diffusion term that degrades roughness. When compared to acoustic data from the 1999 and 2004 Sediment Acoustics Experiments (SAX99 and SAX04), the model yields diffusivities in the range from 3.5 times 10 -11 to 2.5 times 10 -10 m 2 s -1 (from 10 to 80 cm 2 yr -1 ), with the larger values occurring at sites where bottom-feeding fish were active. While the experimental results lend support to the model, a more focused experimental and simulation effort is required to test several assumptions intrinsic to the model.
doi_str_mv 10.1109/JOE.2009.2021287
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subjects Acoustic scattering
Acoustics
Biological system modeling
bioturbation
Degradation
Diffusion
diffusion processes
Equations
Evolution
Evolution (biology)
Fish
Marine
Marine animals
Mathematical models
Roughness
Sea beds
Sea floor roughness
seafloor
sediment transport
Sediments
Surfaces
Testing
Topography
title Acoustic Observation of the Time Dependence of the Roughness of Sandy Seafloors
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