dc.contributor.author | Bratberg, Ivar | |
dc.contributor.author | LePage, Kevin D. | |
dc.contributor.author | Holland, Charles W. | |
dc.contributor.author | Schmidt, Henrik | |
dc.date.accessioned | 2018-10-11T14:09:06Z | |
dc.date.available | 2018-10-11T14:09:06Z | |
dc.date.issued | 2001/05 | |
dc.identifier | 12810 | |
dc.identifier.govdoc | SM-377 | |
dc.identifier.uri | http://hdl.handle.net/20.500.12489/568 | |
dc.description.abstract | OASES 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.format | vi, 44 p. : ill. ; 32 fig. | |
dc.language | English | |
dc.publisher | NATO. SACLANTCEN | |
dc.subject | Acoustic scattering - Seafloor and sea surface | |
dc.subject | OASES (acoustic propagation model) | |
dc.subject | SCARAB (acoustic propagation model) | |
dc.title | Benchmarking of SCARAB volume scattering versus OASES volume scattering | |
dc.type | Scientific Memorandum (SM) | |