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The Seamount as a Diffracting Body

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Bottom-Interacting Ocean Acoustics

Part of the book series: NATO Conference Series ((NATOCS,volume 5))

Abstract

Diffraction over a seamount has been studied by experiments with a three-dimensional physical model of DICKENS seamount. When laboratory diffraction and scattering data are scaled to the ocean and added to absorption and refraction losses at sea, there is excellent agreement with ocean experiments reported by Ebbeson et al. (J. Acoust. Soc. Am. 64, S76 (1978). Both the magnitude and the frequency dependence of the shadowing at sea are predicted over a decade of frequencies.

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References

  1. G. R. Ebbeson, J. M. Tborleifson and R.G. Turner, “Shadowing of sound propagation by a seamount in the northeast Pacific”, J. Acoust. Soc. Am. 64, S76 (1978).

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  9. C. S. Clay and H. Medwin, “Acoustical Oceanography”, Wiley, NewYork (1977). (Ch. 10, Scattering and Reflection of Sound at Rough Surfaces).

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  10. G. R. Ebbeson, Private communication.

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© 1980 Plenum Press, New York

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Medwin, H., Spaulding, R.P. (1980). The Seamount as a Diffracting Body. In: Kuperman, W.A., Jensen, F.B. (eds) Bottom-Interacting Ocean Acoustics. NATO Conference Series, vol 5. Springer, Boston, MA. https://doi.org/10.1007/978-1-4684-9051-0_29

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  • DOI: https://doi.org/10.1007/978-1-4684-9051-0_29

  • Publisher Name: Springer, Boston, MA

  • Print ISBN: 978-1-4684-9053-4

  • Online ISBN: 978-1-4684-9051-0

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