Noise source level density due to surf. II. Duck, NC

For pt.I see ibid., vol.22, no.3, p.425-33 (1997). Ambient noise measurements collected off the coast of Duck, NC, were used in conjunction with modeled transmission loss (TL) and estimated ambient noise due to wave-breaking to generate estimates of spectral source level densities (per meter of surf zone) of surf-generated ambient noise. Estimates of both continuous (local) and discrete (distant) components of noise intensity due to breaking waves were subtracted from the total measured noise field in order to determine the contribution of the noise from the surf zone. Data for two days, representing high sea-state conditions, are presented. Estimated noise source level densities for heavy surf at Duck, NC, varied from 120 to 125 dB re 1 /spl mu/Pa/Hz/sup 1/2//m at 200 Hz to 90-100 dB re 1 /spl mu/Pa/Hz/sup 1/2//m at 900 Hz, with a slope of -5 dB per octave. Results compare well with previous surf noise studies conducted in Monterey Bay as reported in the companion paper by Wilson et al.

[1]  E. Hamilton Geoacoustic modeling of the sea floor , 1980 .

[2]  Sea surface sound : natural mechanisms of surface generated noise in the ocean , 1988 .

[3]  W. Kuperman,et al.  A shallow water experiment to determine the source spectrum level of wind‐generated noise , 1985 .

[4]  B. Kerman Natural Physical Sources of Underwater Sound , 1993 .

[5]  S. Williams,et al.  Physiographic and geological setting of the coastal engineering research center's field research facility , 1989 .

[6]  David M. Farmer,et al.  An Evaluation of the WOTAN Technique of Inferring Oceanic Winds from Underwater Ambient Sound , 1990 .

[7]  Ronald A. Wagstaff,et al.  An Ambient-Noise Model That Includes Coherent Hydrophone Summation for Sonar System Performance in Shallow Water , 1983 .

[8]  S. Wolf,et al.  Site dependence of wind‐dominated ambient noise in shallow water , 1989 .

[9]  P. Wille,et al.  Measurements on the origin of the wind-dependent ambient noise variability in shallow water , 1984 .

[10]  W. Pierson,et al.  A proposed spectral form for fully developed wind seas based on the similarity theory of S , 1964 .

[11]  O. B. Wilson,et al.  Noise source level density due to surf. I. Monterey Bay, CA , 1997 .

[12]  R. M. Hamson The theoretical responses of vertical and horizontal line arrays to wind‐induced noise in shallow water , 1985 .

[13]  G. H. Johnson,et al.  Late Quaternary Stratigraphy of the Inner Virginia Continental Shelf: A Proposed Standard Section: Reply , 1972 .

[14]  W. D. Wilson,et al.  Speed of Sound in Sea Water as a Function of Temperature, Pressure, and Salinity , 1960 .

[15]  O. B. Wilson,et al.  Measurements of acoustic ambient noise in shallow water due to breaking surf , 1982 .

[16]  Michael D. Collins,et al.  Applications and time‐domain solution of higher‐order parabolic equations in underwater acoustics , 1989 .