Large Amplitude Breaking Internal Solitary Waves: Their Origin and Dynamics

Abstract

The long-term goal is to determine the mechanisms of generation, propagation, dissipation, mixing and decay of large amplitude internal waves formed by tidal flow past topography. 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. 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, 2003
Accession Number
ADA629108

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

  • Amplitude
  • Coastal Engineering
  • Computational Science
  • Demographic Cohorts
  • Dissipation
  • Dynamics
  • Electrical Solitons
  • Flow
  • High Resolution
  • Internal Waves
  • Leading Edges
  • Remote Sensing
  • Rhode Island
  • Solitons
  • Tidal Currents
  • Topography
  • Waves

Fields of Study

  • Physics

Readers

  • Atmospheric Science / Meteorology, specifically Wind Wave Turbulence.
  • Marine Ecotoxicology