Relating Ocean Acoustic Ambient to Ocean Surface Dynamics

Abstract

The acoustical significance of ocean surface dynamics is well known. Motivation for establishing the casual relations between these two physical processes has both underwater acoustic system noise reduction and oceanographic remote sensing objectives. The goal has eluded investigators because of the complexity of both the acoustic and oceanographic mechanisms involved. The work discussed here continues progression in spatial scales by utilizing a relatively deep water basin (The Tongue of the Ocean, the Bahamas) in a quasi-controlled environment which made a broadband measurement (40 to 4000 Hz) of the vertical directional spectrum are dominated by local (fetch limited) water surface conditions over a wide range of environmental conditions. While the exploratory nature of the experiment limited the amount of supporting meteorological and oceanographic measurements made, the results give additional credence to the role of entrapped air bubbles and bubble clouds in the generation of acoustic ambient. Sea surface-generated acoustics is shown to be dependent on a fundamental nondimensional variable describing the air-sea boundary process and the rate of energy dissipation caused by wave-breaking in the gravity wave equilibrium range.

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Document Details

Document Type
Technical Report
Publication Date
May 29, 1991
Accession Number
ADA237167

Entities

People

  • R. M. Kennedy

Organizations

  • Naval Undersea Warfare Center

Tags

Communities of Interest

  • Energy and Power Technologies

DTIC Thesaurus Topics

  • Abstracts
  • Acoustics
  • Air Entrainment
  • Classification
  • Drainage Basins
  • Dynamics
  • Energy
  • Frequency
  • Gravity Waves
  • Measurement
  • Oceans
  • Security
  • Surface Properties
  • Surface Tension
  • Test And Evaluation
  • Water
  • Waves

Fields of Study

  • Environmental science

Readers

  • Atmospheric Science / Meteorology, specifically Wind Wave Turbulence.
  • Coastal Oceanography
  • Theoretical Analysis.