Long Nonlinear Internal Waves and Quasi-Steady Lee Waves.

Abstract

Previous observation of large amplitude internal gravity waves generated by tidal flow over a submarine ridge in Massachusetts Bay have motivated the author to consider the general problem of internal gravity wave generation by time-dependent flow of a stratified, inviscid fluid over topography. An internal Korteweg and deVries type equation for the stream function is derived using a three parameter expansion method, where the three small parameters correspond to nonlinear, dispersive, and non-Boussinesq effects. Simple analytic models and laboratory experiments are used to examine mixing and the generation of quasi-steady lee waves. A tall, rapidly oscillating ridge acts to mix the stratified fluid near the ridge; the circulation set up by the collapse of the mixed fluid is determined. In the second study, ray theory is used to analyse lee waves generated behind a low ridge being slowly towed periodically through a stratified fluid. (Author)

Document Details

Document Type
Technical Report
Publication Date
Jun 01, 1972
Accession Number
AD0746137

Entities

People

  • Chi-yuan Lee

Organizations

  • Massachusetts Institute of Technology

Tags

DTIC Thesaurus Topics

  • Demographic Cohorts
  • Gravity
  • Gravity Waves
  • Internal Waves
  • Landforms
  • Massachusetts Bay
  • Ridges
  • Stratified Fluids
  • Topography
  • Waves

Fields of Study

  • Mathematics

Readers

  • Atmospheric Science / Meteorology, specifically Wind Wave Turbulence.