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Volume 133, Issue 5_Supplement
May 2013

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May 01 2013


WIND-DEPENDENCE OF LOW-FREQUENCY AMBIENT NOISE IN THE DEEP-OCEAN SOUND CHANNEL

Stephen Nichols;
Stephen Nichols
Grad. Prog. in Acoust., The Penn State Univ., 201 Appl. Sci. Bldg., State
College, PA 16802smn5198@psu.edu
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David L. Bradley
David L. Bradley
Appl. Res. Lab., The Penn State Univ., State College, PA
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J. Acoust. Soc. Am. 133, 3396 (2013)
https://doi.org/10.1121/1.4805902

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Citation

Stephen Nichols, David L. Bradley; Wind-dependence of low-frequency ambient
noise in the deep-ocean sound channel. J. Acoust. Soc. Am. 1 May 2013; 133
(5_Supplement): 3396. https://doi.org/10.1121/1.4805902

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In the low-frequency range (1–125 Hz), the deep-ocean ambient noise field is
produced by seismic, marine life, ship traffic, and wind-dependent hydrodynamic
noise mechanisms. This study focuses on the contribution of wind-related source
mechanisms to the overall ambient noise field, as well as previous attempts to
understand the physics of these mechanisms. The Comprehensive Nuclear-Test Ban
Treaty Organization (CTBTO) hydroacoustic monitoring system has produced nearly
continuous recordings of the low-frequency deep-ocean ambient noise field at
sites in the Pacific, Atlantic, and Indian Oceans, each spanning several years
in length. Additionally, wind speed data have been recorded at the host island
of each station by the National Oceanic and Atmospheric Administration (NOAA).
Correlation techniques are used with these two datasets to determine the
relationship between wind speed and the sound level in different frequency
bands, and to determine the prominence of wind-related noise in the combined
ambient noise spectrum. Results from the three sites are compared to each other
to assess the uniformity of wind-generated noise over the world’s ocean basins.

Topics
Underwater acoustics, Acoustic noise, Acoustical oceanography, Oceans,
Electronic noise, Nuclear weapon testing

© 2013 Acoustical Society of America.
2013
Acoustical Society of America



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