Mixing in Symmetric Holmboe Waves

Author:

Smyth W. D.1,Carpenter J. R.2,Lawrence G. A.2

Affiliation:

1. College of Oceanic and Atmospheric Sciences, Oregon State University, Corvallis, Oregon

2. Department of Civil Engineering, University of British Columbia, Vancouver, British Columbia, Canada

Abstract

Abstract Direct simulations are used to study turbulence and mixing in Holmboe waves. Previous results showing that mixing in Holmboe waves is comparable to that found in the better-known Kelvin–Helmholtz (KH) billows are extended to cover a range of stratification levels. Mixing efficiency is discussed in detail, as are effective diffusivities of buoyancy and momentum. Entrainment rates are compared with results from laboratory experiments. The results suggest that the ratio of the thicknesses of the shear layer and the stratified layer is a key parameter controlling mixing. With that ratio held constant, KH billows mix more rapidly than do Holmboe waves. Among Holmboe waves, mixing increases with increasing density difference, despite the fact that the transition to turbulence is delayed or prevented entirely by the stratification. Results are summarized in parameterizations of the effective viscosity and diffusivity of Holmboe waves.

Publisher

American Meteorological Society

Subject

Oceanography

Reference28 articles.

1. On Holmboe’s instability for smooth shear and density profiles.;Alexakis;Phys. Fluids,2005

2. Evolution and mixing of asymmetric Holmboe instabilities.;Carpenter;J. Fluid Mech.,2007

3. Anatomy of the mixing transition in homogeneous and stratified free shear layers.;Caulfield;J. Fluid Mech.,2000

4. On the behaviour of symmetric waves in stratified shear layers.;Holmboe;Geophys. Publ.,1962

5. The influence of stratification on secondary instability in free shear layers.;Klaassen;J. Fluid Mech.,1991

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