Published In

Journal of the Acoustical Society of America

Document Type

Article

Publication Date

11-2009

Subjects

Underwater acoustics, Acoustical engineering, Noise -- Measurement

Abstract

Recently, a method has been developed that exploits the correlation properties of the ocean’s ambient noise to measure water depth (a passive fathometer) and seabed layering [M. Sideriuset al., J. Acoust. Soc. Am.120, 1315–1323 (2006)]. This processing is based on the cross-correlation between the surface noise and the echo return from the seabed. To quantitatively study the dependency between processing and environmental factors such as wind speed, measurements were made using a fixed hydrophone array while simultaneously characterizing the environment. The measurements were made in 2006 in the shallow waters (25m)approximately 75km off the coast of Savannah, GA. A Navy tower about 100m from the array was used to measure wind speed and to observe the sea-surface using a video camera. Data were collected in various environmental conditions with wind speeds ranging from 5 to 21m/s and wave heights of 1–3.4m. The data are analyzed to quantify the dependency of passive fathometer results on wind speeds, wave conditions, and averaging times. One result shows that the seabed reflection is detectable even in the lowest wind conditions. Further, a technique is developed to remove the environmental dependency so that the returns estimate seabed impedance.

Description

This is the publisher's final PDF. © 2009 U.S. Government. 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. 126, 2234 and may be found at: http://dx.doi.org/10.1121/1.3216915

DOI

10.1121/1.3216915

Persistent Identifier

http://archives.pdx.edu/ds/psu/12120

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