Long-Range Shallow-Water Propagation Loss Fluctuations,

Abstract

One of the most striking features of the long-range shallow-water propagation of sonic frequencies is the fluctuation of the received signals. When a steady single-frequency tone is transmitted, the received signal level will vary over a range as much as 50-db. The fluctuation characteristics of a typical record of received sound were studied to yield information about: (1) the amplitude distribution functions, (2) the cross-correlations between signals received at different hydrophones, and (3) the autocorrelations and power spectra of the signal envelopes. The shallow water results presented are for an almost ideal flat 60-fathom sand bottom at ranges of 10, 15, 20, and 30 kyd for frequencies of 350, 700, 1200, and 2,400 cps; and for a 50-fathom nondepositional miocene sandstone bottom at ranges of 4, 8, 16, and 25 kyds for frequencies of 700 and 1200 cps; and, at ranges of 4 and 16 kyds for frequencies of 1200 and 2,400 cps.

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Document Details

Document Type
Technical Report
Publication Date
Jan 01, 1958
Accession Number
ADA066694

Entities

People

  • K. V. Mackenize

Organizations

  • Navy Electronics Laboratory

Tags

Communities of Interest

  • Advanced Electronics
  • Ground and Sea Platforms

DTIC Thesaurus Topics

  • Coefficients
  • Cross Correlation
  • Data Analysis
  • Data Science
  • Distribution Functions
  • Frequency
  • Hydrophones
  • Information Science
  • Intervals
  • Power Spectra
  • Sand
  • Shallow Water
  • Spectra
  • Water

Fields of Study

  • Physics

Readers

  • Acoustics.
  • Oceanography.
  • Radar Systems Engineering.