Published In

Journal of the Acoustical Society of America

Document Type

Article

Publication Date

4-2010

Subjects

Underwater acoustics, Noise, Geologic Sediments, Acoustical engineering

Abstract

Recently, a technique has been developed to image seabed layers using the ocean ambient noise field as the sound source. This so called passive fathometer technique exploits the naturally occurring acoustic sounds generated on the sea-surface, primarily from breaking waves. The method is based on the cross-correlation of noise from the ocean surface with its echo from the seabed, which recovers travel times to significant seabed reflectors. To limit averaging time and make this practical, beamforming is used with a vertical array of hydrophones to reduce interference from horizontally propagating noise. The initial development used conventional beamforming, but significant improvements have been realized using adaptive techniques. In this paper, adaptive methods for this process are described and applied to several data sets to demonstrate improvements possible as compared to conventional processing.

Description

This is the publisher's final PDF. Copyright 2010 Acoustical Society of America. This article may be downloaded for personal use only. Any other use requires prior permission of the author and the Acoustical Society of America. The following article appeared in J. Acoust. Soc. Am. 127, 2193 and may be found at: http://dx.doi.org/10.1121/1.3303985

DOI

10.1121/1.3303985

Persistent Identifier

http://archives.pdx.edu/ds/psu/12072

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