Large Amplitude Breaking Internal Waves: Their Origin and Dynamics

Abstract

LONG-TERM GOALS. To determine the mechanisms of generation, propagation, dissipation, mixing and decay of large amplitude internal waves formed by tidal flow past topography. OBJECTIVES. Our objectives are to use both acoustic remote sensing and in situ profile observations of large amplitude internal waves, together with highly resolved numerical simulation, so as to develop a predictive understanding of their behavior, with application to their generation by flow past topography, their contribution to mass and momentum transport, mixing, modulation of near surface bubble clouds and related properties, including the subduction of bubbles and their fate in the presence of large amplitude streamline deformations trapped behind sills, before their release as freely propagating internal waves. A further objective is to use the numerical simulation to test hypotheses related to observed convective overturning and shear instability induced by the waves under different conditions of stratification and shear and to estimate the mixing and dissipation resulting from these processes.

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Document Details

Document Type
Technical Report
Publication Date
Sep 30, 2006
Accession Number
ADA629966

Entities

People

  • David M. Farmer

Organizations

  • University of Rhode Island

Tags

Communities of Interest

  • Energy and Power Technologies
  • Ground and Sea Platforms

DTIC Thesaurus Topics

  • Acoustic Scattering
  • Amplitude
  • Coastal Engineering
  • Demographic Cohorts
  • Dynamics
  • Electrical Solitons
  • Frequency
  • High Resolution
  • Instability
  • Internal Waves
  • Rhode Island
  • Solitons
  • Sonar
  • South China Sea
  • Stratified Fluids
  • Topography
  • Waves

Fields of Study

  • Physics

Readers

  • Fluid Mechanics and Fluid Dynamics.
  • Ocean-Atmosphere Mesoscale Modeling, Data Assimilation, and Flux Boundary Layers