Benthic Tubulence and Mixing Induced by Nonlinear Internal Waves

Abstract

The transition to a primary instability in the footprint of nonlinear internal waves of depression was investigated using spectral multidomain-based numerical simulations. The fully nonlinear internal wave fields were supplied through a highly nonlinear extended Korteweg De Vries algorithm generated by Sakai & Redekopp (2007). Results were qualitatively similar to the findings of Diamessis and Redekopp (2006). In the absence of an oncoming current, no transition was observed. Introducing a current and with a sufficiently strong wave amplitude and Reynolds number, the separated bottom boundary layer under the wave and behind its trough experienced a shear instability, accompanied by vortex shedding, powerful bottom shear-stresses and strong near-bed vertical velocities, indicating potential for resuspension. The vortex shedding was intermittent, consisting of bursts of 5-6 eject vortices alternating with calm periods. A subcritical nonlinear transition to turbulence was also identified and is currently under investigation.

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Document Details

Document Type
Technical Report
Publication Date
Mar 31, 2010
Accession Number
ADA520127

Entities

People

  • Peter J Diamessis

Organizations

  • Cornell University College of Engineering

Tags

Communities of Interest

  • Energy and Power Technologies

DTIC Thesaurus Topics

  • Boundary Layer
  • Computational Fluid Dynamics
  • Flow
  • Fluid Dynamics
  • Fluid Flow
  • Fluid Mechanics
  • Internal Waves
  • Layers
  • Mechanical Properties
  • Physics Laboratories
  • Reynolds Number
  • Stratified Fluids
  • Three Dimensional
  • Turbulence
  • Turbulent Mixing
  • Two Dimensional
  • Vortex Shedding

Fields of Study

  • Physics

Readers

  • Atmospheric Science / Meteorology, specifically Wind Wave Turbulence.
  • Coastal Oceanography
  • Fluid Mechanics and Fluid Dynamics.