Reconstruction of sea bottom acoustic parameters using a multilayer model and obliquely incident acoustic waves

Frangos, P; Aliferis, Y; Danaka, K; Athanassoulis, G

dc.contributor.author	Frangos, P	en
dc.contributor.author	Aliferis, Y	en
dc.contributor.author	Danaka, K	en
dc.contributor.author	Athanassoulis, G	en
dc.date.accessioned	2014-03-01T02:41:16Z
dc.date.available	2014-03-01T02:41:16Z
dc.date.issued	1996	en
dc.identifier.uri	https://dspace.lib.ntua.gr/xmlui/handle/123456789/30438
dc.subject	Acoustic Waves	en
dc.subject.other	Acoustic wave reflection	en
dc.subject.other	Acoustic wave scattering	en
dc.subject.other	Algorithms	en
dc.subject.other	Electromagnetism	en
dc.subject.other	Interfaces (materials)	en
dc.subject.other	Mathematical models	en
dc.subject.other	Recursive functions	en
dc.subject.other	Abstract only	en
dc.subject.other	Inverse scattering method (ISM)	en
dc.subject.other	Multilayer models	en
dc.subject.other	Obliquely incident acoustic waves	en
dc.subject.other	Sea bottom acoustic parameters	en
dc.subject.other	Underwater acoustics	en
dc.title	Reconstruction of sea bottom acoustic parameters using a multilayer model and obliquely incident acoustic waves	en
heal.type	conferenceItem	en
heal.identifier.primary	10.1109/AEM.1996.873170	en
heal.identifier.secondary	http://dx.doi.org/10.1109/AEM.1996.873170	en
heal.publicationDate	1996	en
heal.abstract	An inverse scattering method (ISM) for the reconstruction of sea bottom acoustic parameters, such as acoustic speed and density, is presented. The model assumes that the sea bottom is made up of N layers, the last one having infinite thickness. The method is based on an iterative technique for the case of the corresponding electromagnetic (EM) problem, where the layers' permittivities are reconstructed from EM field reflection data.	en
heal.publisher	IEEE	en
heal.journalName	Trans Black Sea Region Symposium on Applied Electromagnetism	en
dc.identifier.doi	10.1109/AEM.1996.873170	en