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dc.contributor.authorGingras, Donald F.
dc.date.accessioned2018-10-11T14:06:53Z
dc.date.available2018-10-11T14:06:53Z
dc.date.issued1995/10
dc.identifier2014
dc.identifier.govdocSR-236
dc.identifier.urihttp://hdl.handle.net/20.500.12489/306
dc.description.abstractNormal mode theory is used to illustrate that a vertical array of weighted sources driven in an
dc.description.abstractappropriate frequency band can be used to minimize the combined effects of attenuation and bottomgenerated backscatter in shallow water. Results are presented for three canonical geoacoustic
dc.description.abstractmodels using both a winter and summer sound speed profile. It is shown that through selective
dc.description.abstractexcitation of only mode 1 there exists an optimum frequency band providing both minimum attenuation and minimum bottom-generated backscatter. The results indicate that the center frequency of the optimum band increases as the critical angle decreases.
dc.format33 p. : ill. ; 13 fig.
dc.languageEnglish
dc.publisherNATO. SACLANTCEN
dc.relation.ispartofseriesADB208381
dc.subjectAcoustic scattering
dc.subjectSeafloor
dc.subjectShallow water
dc.titleSingle mode excitation, attenuation and backscatter in shallow water
dc.typeScientific Report (SR)


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