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A Propagation Anomaly Observed in the Barents Sea

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Ocean Seismo-Acoustics

Part of the book series: NATO Conference Series ((MARS,volume 16))

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Abstract

A low frequency sound propagation experiment was conducted in the Western Barents Sea from a towed continuous sound source and air-dropped explosive sound sources to a hydrophone lying on the sea bed. Anomalies in the propagation results were traced to sub-bottom features, in particular to a region of basement outcrop. This paper will present data suggesting the influence of a particular salt diapir occurring within this basement outcrop region upon the low frequency sound propagation. The results suggest alternative interpretations for the mechanism of influence of the sea-bed upon the sound field.

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References

  1. R. Chapman and G. Ebbeson, Acoustic Shadowing by an Isolated Seamount, J. Acoust. Soc. Am. 73: 1979 (1983).

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  2. H. Medwin and R. Spaulding, The Seamount as a diffracting body. In: Bottom-Interacting Ocean Acoustics. W. Kuperman and F.B. Jensen eds. Plenum Press, New York, NY p. 421 (1980).

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  3. P. Rona, Evaporities at Passive Margins, Atlantic Oceanographic and Meteorological Laboratories, NOA, Miami, Florida.

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  4. J. Faleide and S. Gudlaugsson, Geology of the Western Barents Sea, Cand Royal Thesis in Applied Geophysics, Dept. of Geology, University of Oslo 1981.

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© 1986 Plenum Press, New York

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Hug, E.H. (1986). A Propagation Anomaly Observed in the Barents Sea. In: Akal, T., Berkson, J.M. (eds) Ocean Seismo-Acoustics. NATO Conference Series, vol 16. Springer, Boston, MA. https://doi.org/10.1007/978-1-4613-2201-6_22

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  • DOI: https://doi.org/10.1007/978-1-4613-2201-6_22

  • Publisher Name: Springer, Boston, MA

  • Print ISBN: 978-1-4612-9293-7

  • Online ISBN: 978-1-4613-2201-6

  • eBook Packages: Springer Book Archive

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