Surface wave, internal wave, and source motion effects on matched field processing in a shallow water waveguide

dc.contributor.author Daugherty, John R.
dc.date.accessioned 2012-09-21T19:00:10Z
dc.date.available 2012-09-21T19:00:10Z
dc.date.issued 1989-08
dc.description Submitted in partial fulfillment of the requirements for the degree of Master of Science at the Massachusetts Institute of Technology and the Woods Hole Oceanographic Institution August 1989 en_US
dc.description.abstract Given well known environmental conditions, matched field processing has been shown to be a promising signal processing technique for the localization of acoustic sources. However, when environmental data are incomplete or inaccurate, a 'mismatch' occurs between the measured field and model field which can lead to a severe degradation of the localization estimator. We investigate the possible mismatch effects of surface and internal waves on matched field processing in a shallow water waveguide. We utilize a modified ray theory, based on the work of Tindle, to calculate the acoustic pressure field. This allows us to simply incorporate range dependent environmental conditions as well as to generalize our work to deeper waveguides. In general, the conventional (Bartlett) matched field beamformer does not provide sufficient resolution to unambiguously locate a source, even in a perfectly matched environment. The maximum likelihood method (MLM) matched field beamformer has much better resolution but is extremely susceptible to mismatch. The mismatch due to surface roughness can result in a large reduction of the estimator peak. Part, but not all, of the peak can be regained by 1)using a model which includes incomplete reflection at the surface based on actual sea surface statistics and 2) short time averaging of the measured signal, with times on the order of the period of the surface waves. Mismatch due to internal waves can also result in a large degradation of the estimator. Averaging over the same time period as surface waves provides little improvement and leads one to surmise that internal waves may be a limiting constraint on matched field processing. Finally, we combine the surface and internal wave fields with a slowly moving source. This example highlights the necessity for the development of a beamformer which has a broader mainlobe while maintaining adequate sidelobe suppression, and we address this issue by looking at two such beamformers. en_US
dc.format.mimetype application/pdf
dc.identifier.citation Daugherty, J. R. (1989). Surface wave, internal wave, and source motion effects on matched field processing in a shallow water waveguide [Doctoral thesis, Massachusetts Institute of Technology and Woods Hole Oceanographic Institution]. Woods Hole Open Access Server. https://doi.org/10.1575/1912/5386
dc.identifier.doi 10.1575/1912/5386
dc.identifier.uri https://hdl.handle.net/1912/5386
dc.language.iso en_US en_US
dc.publisher Massachusetts Institute of Technology and Woods Hole Oceanographic Institution en_US
dc.relation.ispartofseries WHOI Theses en_US
dc.subject Internal waves en_US
dc.subject Surface waves en_US
dc.title Surface wave, internal wave, and source motion effects on matched field processing in a shallow water waveguide en_US
dc.type Thesis en_US
dspace.entity.type Publication
relation.isAuthorOfPublication 496536f0-1726-4824-8c3d-bd6c53f00ca9
relation.isAuthorOfPublication.latestForDiscovery 496536f0-1726-4824-8c3d-bd6c53f00ca9
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