An Experimental Study of a Method to Attenuate Surface Waves Over a Limited Region of the Open Ocean.

Abstract

An experimental investigation of the refraction of surface gravity waves by relatively narrow (of the order of or less than one wave length) and shallow, laterally sheared, surface currents was undertaken to determine the feasibility of employing artificially-generated currents to achieve local wave damping in the ocean. In the experiments, single frequency wave trains (wave length, wave length sub 0, in still water) were initially propagated in the same direction as the direction of the current in the wake of a towed grid (with lateral extent, W sub g, and draft, d sub g). The required power for wave lengths up to 300 feet was within the range of installed power of conventional off-shore boats.

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Document Details

Document Type
Technical Report
Publication Date
Jun 01, 1978
Accession Number
ADA056282

Entities

People

  • Richard I. Hires

Organizations

  • Stevens Institute of Technology

Tags

DTIC Thesaurus Topics

  • Boundaries
  • California
  • Coefficients
  • Contracts
  • Deep Water
  • Flow
  • Frequency
  • Froude Number
  • Hydrodynamics
  • Measurement
  • New Jersey
  • Regions
  • Surface Waves
  • United States
  • Water Waves
  • Wave Power
  • Waves

Fields of Study

  • Physics

Readers

  • Atmospheric Science / Meteorology, specifically Wind Wave Turbulence.