Finite-Amplitude Solitary Water Waves.

Abstract

This paper considers the existence problem for solutions of the free boundary value problem which arises from the question of the existence of solitary gravity waves, moving without changes of form, and with constant velocity, on the surface of ideal fluid in a horizontal canal of finite depth. The analysis imposes no restriction on either the slope or the amplitude of the wave, and we prove that there exists a connected set of solitary waves containing waves of all slope between 0 and pi/6. It is then proved that each of these solitary waves has finite mass, and, as a consequence, that F > 1, where F is the Froude number. This, in turn, tells us that the solitary wave decays faster than exp(-alpha abs.val.(x/h), where alpha is an element or (0, alpha-bar) and 1/alpha-bar tam(alph-bar) = f-squared. Finally, it is shown that, in a certain limit, these solitary waves converge to a solitary stokes wave of greatest height, and the validity of stokes' conjecture for solitary waves is considered, but not resolved. (Author)

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Document Details

Document Type
Technical Report
Publication Date
Oct 01, 1979
Accession Number
ADA079718

Entities

People

  • C. J. Amick
  • J. F. Toland

Organizations

  • University of Wisconsin–Madison

Tags

Communities of Interest

  • Air Platforms
  • Energy and Power Technologies

DTIC Thesaurus Topics

  • Analytic Functions
  • Banach Space
  • Boundary Value Problems
  • Computational Science
  • Equations
  • Fluid Mechanics
  • Froude Number
  • Gravity Waves
  • Integral Equations
  • Integrals
  • Mathematics
  • Mechanics
  • Sequences
  • Solitons
  • Stratified Fluids
  • United States
  • Water Waves

Fields of Study

  • Mathematics

Readers

  • Atmospheric Science / Meteorology, specifically Wind Wave Turbulence.
  • Calculus or Mathematical Analysis