Evolution of Weakly Nonlinear Water Waves in the Presence of Viscosity and Surfactant

Abstract

Amplitude evolution equations are derived for viscous gravity waves and for viscous capillary-gravity waves with surfactants in water of infinite depth. Multiple scales are used to describe the slow modulation of a wave packet, and matched asymptotic expansions are introduced to represent the viscous boundary layer at the free surface. The resulting dissipative nonlinear Schrodinger equations show that the largest terms in the damping coefficients are unaltered from previous linear results up to third order in the amplitude expansions. The modulational instability of infinite wavetrains of small but finite amplitude is studied analytically and computationally. For capillary-gravity waves a band of Weber numbers is found in which the linear analysis guarantees neutral stability in the absence of viscous dissipation. The corresponding spectral computation shows modulation features that represent a small-amplitude recurrence not directly related to the Benjamin-Feir instability.

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Document Details

Document Type
Technical Report
Publication Date
Aug 14, 1989
Accession Number
ADA250962

Entities

People

  • A. F. Messiter
  • S. W. Joo
  • W. W. Schultz

Organizations

  • University of Michigan

Tags

Communities of Interest

  • C4I
  • Ground and Sea Platforms
  • Space

DTIC Thesaurus Topics

  • Boundary Layer
  • Capillary Waves
  • Coordinate Systems
  • Differential Equations
  • Electrical Solitons
  • Engineering
  • Equations
  • Frequency
  • Frequency Shift
  • Hydrodynamics
  • Inviscid Flow
  • Marine Engineering
  • Mechanics
  • Naval Architecture
  • Surface Tension
  • Two Dimensional
  • Universities

Fields of Study

  • Mathematics
  • Physics

Readers

  • Atmospheric Science / Meteorology, specifically Wind Wave Turbulence.
  • Finite Element Method (FEM) for solving Partial Differential Equations (PDEs)