On the Shore Singularity of Water-Wave Theory. Part 2. Small Waves Don't Break on Gentle Beaches.

Abstract

The model of gravitational surface waves on beaches of small slope formulated in and its mathematical theory are used to show how an incident-wave amplitude can be defined so that a bound on it guarantees solutions which respect the assumptions of the model everywhere and forever. The structure of those solutions far from shore is then compared with that predicted near shore by the classical, linear theory to remove the indeterminacies of both theories: Shore reflection is determined for the classical theory, and it is shown how the critical length scale and amplitude of the beach theory are related to the familiar wavelength and amplitude in deep water. These results indicate that the beach theory captures and elucidates the basic singularity structure underlying the shore behavior of gravitational surface waves. Keywords: Amplitude bounds; Beach erosion; Army Corps of Engineers. (Author)

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Document Details

Document Type
Technical Report
Publication Date
Oct 01, 1985
Accession Number
ADA163652

Entities

People

  • R. E. Meyer

Organizations

  • University of Wisconsin–Madison

Tags

Communities of Interest

  • Air Platforms
  • Energy and Power Technologies

DTIC Thesaurus Topics

  • Amplitude
  • Beaches
  • Bessel Functions
  • Deep Water
  • Elevation
  • Engineering
  • Equations
  • Frequency
  • Geographic Regions
  • Mathematics
  • Numbers
  • Shores
  • Standing Waves
  • Two Dimensional
  • United States
  • Water Waves
  • Waves

Readers

  • Atmospheric Science / Meteorology, specifically Wind Wave Turbulence.
  • Calculus or Mathematical Analysis
  • Coastal and Marine Engineering/Sediment Transport/Hydraulic Engineering