A LABORATORY EXPERIMENT ON SURFACE WAVE ATTENUATION DUE TO UNDERWATER TURBULENCE.

Abstract

The attenuation of surface waves caused by underwater turbulence was investigated in a wave-tank experiment. The waves studied (frequencies ranging from 1.2 to 12.3 Hertz) were strongly attenuated by a zone of grid-generated turbulence. This attenuation depended on the length of the turbulent region, and on the frequency of the incident wave. The equation governing attenuation was: h = h sub 0 exp(-ax) where h is wave height, h sub 0 is undisturbed wave height, x is the length of the turbulent region, and a is an attenuation coefficient proportional to the cube root of frequency. It was also noted that the waves were shifted in phase as they passed through the turbulence, and that the magnitude of this shift increased with frequency. The quantitative results of the experiment were obtained from measurements of nearly sinusoidal waves. They were confirmed, qualitatively, for a continuous spectrum of waves by measurement of wind-generated model sea surface. (Author)

Document Details

Document Type
Technical Report
Publication Date
Dec 01, 1968
Accession Number
AD0686655

Entities

People

  • James Edward Paquin

Organizations

  • Naval Postgraduate School

Tags

DTIC Thesaurus Topics

  • Attenuation
  • Buildings And Structures
  • Coefficients
  • Continuous Spectra
  • Equations
  • Frequency
  • Frequency Shift
  • Measurement
  • Research Facilities
  • Spectra
  • Surface Waves
  • Turbulence
  • Waves

Readers

  • Atmospheric Science / Meteorology, specifically Wind Wave Turbulence.

Technology Areas

  • AI & ML