The Interaction of Waves and Turbulence in Water

Abstract

The report investigates a system in which water waves are generated and propagated in a turbulent flow field. Growth of wind wave spectra and decay of monochromatic waves are considered. For monochromatic waves the turbulence in the water can greatly increase the rate of wave energy dissipation and that the data can be fitted by an equation with an eddy viscosity term proportional to the wave height, the phase speed of the waves, and the intensity of the larger scale turbulence. Growth of wind waves on turbulent water is faster than in still water; however, maximum wave height in turbulent water is always lower than in still water. Wave energy spectra at the longer fetches in turbulent water show more wave energy at low frequency and less at high frequency than those for still water. Turbulence in water alters the rate of transfer of energy from the wind to the waves, the maximum height allowed and the distribution of wave energy among the various frequencies.

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Document Details

Document Type
Technical Report
Publication Date
Jun 01, 1972
Accession Number
AD0754645

Entities

People

  • John D. Skoda

Organizations

  • University of California, Berkeley

Tags

DTIC Thesaurus Topics

  • Abstracts
  • California
  • Digital Data
  • Doppler Effect
  • Elastic Waves
  • Electronic Equipment
  • Energy Transfer
  • Engineering
  • Equations
  • Flow Fields
  • Frequency
  • Gravity Waves
  • Hydraulic Engineering
  • Literature Surveys
  • Measurement
  • Particles
  • Recording Systems
  • Resistance
  • Standing Waves
  • Universities
  • Water Waves

Fields of Study

  • Physics

Readers

  • Marine Hydrodynamics
  • Ocean-Atmosphere Mesoscale Modeling, Data Assimilation, and Flux Boundary Layers
  • Plasma Physics / Magnetohydrodynamics