Vertical Shear Plus Horizontal Stretching as a Route to Mixing

Abstract

The combined effect of vertical shear and horizontal stretching leads to thin, sloping structures in tracer fields, whose vertical length scale is much smaller than their horizontal length scale. These structures are then vulnerable to vertical mixing processes. This effect needs to be taken into account when interpreting the horizontal structure of oceanic (and atmospheric) tracers and may explain recent oceanographic observations.

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Document Details

Document Type
Technical Report
Publication Date
Jan 19, 2001
Accession Number
ADP013582

Entities

People

  • Peter H. Haynes

Organizations

  • University of Cambridge

Tags

Communities of Interest

  • Materials and Manufacturing Processes

DTIC Thesaurus Topics

  • Advection
  • Applied Mathematics
  • Aspect Ratio
  • Diffusion
  • Diffusivity
  • Equations
  • Flow
  • Mixing
  • Probability
  • Statistics
  • Steady Flow
  • Stratified Fluids
  • Three Dimensional
  • Turbulence
  • Turbulent Flow
  • Turbulent Mixing
  • Two Dimensional

Fields of Study

  • Environmental science

Readers

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