Bottom Reverberation Measurements in the Norwegian Sea and North Atlantic Ocean.

Abstract

Measurements of bottom reverberation were made at six locations in the Norwegian Sea and North Atlantic Ocean, and scattering strengths determined for grazing angles between 83 deg 30 min and 35 deg 30 min, and one-third octave frequencies from 2.5 to 12.5 kHz. In general, the data are consistent with the concept of Volovova and Zhitovskiy (1965), in which the bottom is considered to be composed of roughness elements much greater and much smaller than the wavelengths of the incident sound, with each type of roughness producing characteristic effects in the reverberation. Among these effects, evident in the analyzed data, are a small dependence of scattering strength on frequency at high grazing angles, and a greater dependence at low grazing angles. Scattering strengths at the higher frequencies do not decrease as much with decreasing grazing angles as do those at the lower frequencies. Standard deviations of scattering strengths are greatest at high grazing angles and low frequencies. Contrary to the data presented by Randlett and Urick (1968), no clear relationships between bottom scattering strength and physiographic province are evident, but this is perhaps due to the small number of stations studied. (Author)

Document Details

Document Type
Technical Report
Publication Date
Mar 21, 1969
Accession Number
AD0852507

Entities

People

  • Peter B. Schmidt

Organizations

  • Naval Oceanographic Office

Tags

DTIC Thesaurus Topics

  • Atlantic Ocean
  • Frequency
  • Grazing
  • Grazing Angles
  • Measurement
  • North Atlantic Ocean
  • Norwegian Sea
  • Oceans
  • Reverberation
  • Roughness
  • Scattering

Fields of Study

  • Geology

Readers

  • Acoustics.
  • Oceanography.
  • Solar Physics