AN OVERVIEW OF MATCHED-FIELD METHODS IN OCEAN ACOUSTICS

Citation
Ab. Baggeroer et al., AN OVERVIEW OF MATCHED-FIELD METHODS IN OCEAN ACOUSTICS, IEEE journal of oceanic engineering, 18(4), 1993, pp. 401-424
Citations number
139
Categorie Soggetti
Oceanografhy,"Engineering, Civil","Engineering, Eletrical & Electronic","Engineering, Marine
ISSN journal
03649059
Volume
18
Issue
4
Year of publication
1993
Pages
401 - 424
Database
ISI
SICI code
0364-9059(1993)18:4<401:AOOMMI>2.0.ZU;2-6
Abstract
Recent array processing methods for ocean acoustics have utilized the physics of wave propagation as an integral part of their design. The p hysics of the propagation leads to both improved performance and to al gorithms where the complexity of the ocean environment can be exploite d in ways not possible with traditional plane wave based methods. Matc hed field processing (MFP) is a generalized beamforming method which u ses the spatial complexities of acoustic fields in an ocean waveguide to localize sources in range, depth and azimuth or to infer parameters of the waveguide itself. It has experimentally localized sources with accuracies exceeding the Rayleigh limit for depth and the Fresnel lim it for range by two orders of magnitude. MFP exploits the coherence of the mode/multipath structure and it is especially effective at low fr equencies where the ocean supports coherent propagation over very long ranges. This contrasts with plane wave based models which are degrade d by modal and multipath phenomena and are generally ineffective when waveguide phenomena are important. MFP can have either conventional or adaptive formulations and it has been implemented with an assortment of both narrowband and wideband signal models. All involve some form o f correlation between the replicas derived from the wave equation and the data measured at an array of sensors. One can view MFP as an inver se problem where one attempts to ''invert'' the wave equation for thes e dependencies over the parameter space of the source and the environm ent. There is currently a large literature discussing many theoretical aspects of MFP including numerous simulations; several experiments ac quiring data for MFP now have been conducted in several ocean environm ents and these have demonstrated both its capabilities and some of its limitations. Consequently, there is a modest understanding of both th e theory and the experimental capabilities of MFP. This article provid es an overview of both.