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dc.contributor.authorBratberg, Ivar
dc.contributor.authorLePage, Kevin D.
dc.contributor.authorHolland, Charles W.
dc.contributor.authorSchmidt, Henrik
dc.date.accessioned2018-10-11T14:09:06Z
dc.date.available2018-10-11T14:09:06Z
dc.date.issued2001/05
dc.identifier12810
dc.identifier.govdocSM-377
dc.identifier.urihttp://hdl.handle.net/20.500.12489/568
dc.description.abstractOASES uses wavenumber integration to solve for the backscattered pressure caused by sound speed and density inhomogeneity scatterers in the sediment; SCARAB uses a ray path technique to find the backscattered intensity. This report compares the two models for a variety of sediment backscattering scenarios and identifies situations where the accuracy of SCARAB is compromised.
dc.formatvi, 44 p. : ill. ; 32 fig.
dc.languageEnglish
dc.publisherNATO. SACLANTCEN
dc.subjectAcoustic scattering - Seafloor and sea surface
dc.subjectOASES (acoustic propagation model)
dc.subjectSCARAB (acoustic propagation model)
dc.titleBenchmarking of SCARAB volume scattering versus OASES volume scattering
dc.typeScientific Memorandum (SM)


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