Vertical Noise Directionality in the Deep Ocean: A Review

Abstract

Analysis of data over a wide frequency range (0 Hz to 100 kHz) indicates that three factors play significant roles in determining the vertical directionality of ambient noise in the deep ocean. First is the preponderance of noise sources at or near the ocean surface rather than distributed throughout the water column. Second is the typical deep ocean sound speed profile, which allows high angle arrivals at a receiver only at relatively short ranges. Third is attenuation, which abruptly limits the range that noise is received at a given frequency. These factors result in a transition of higher noise at high angles (short ranges) for high frequencies to higher noise at low angles (long ranges) for low frequencies. A review is made of present results and possible deficiencies.

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Document Details

Document Type
Technical Report
Publication Date
Dec 12, 1985
Accession Number
ADA163386

Entities

People

  • David G. Browning
  • William A. Von Winkle

Organizations

  • Naval Underwater Systems Center

Tags

Communities of Interest

  • Ground and Sea Platforms

DTIC Thesaurus Topics

  • Ambient Noise
  • Atmospheric Motion
  • Attenuation
  • Classification
  • Climate Change
  • Deep Oceans
  • Deep Water
  • Frequency
  • Frequency Domain
  • High Angles
  • Losses
  • Low Angles
  • Oceanography
  • Oceans
  • Security
  • Very Low Frequency
  • Water

Fields of Study

  • Physics

Readers

  • Atmospheric Science / Meteorology, specifically Wind Wave Turbulence.