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Diapycnal mixing of passive tracers by Kelvin–Helmholtz instabilities

Published online by Cambridge University Press:  11 August 2020

Jared Penney Open the ORCID record for Jared Penney [Opens in a new window] ,
Yves Morel Open the ORCID record for Yves Morel [Opens in a new window] ,
Peter Haynes Open the ORCID record for Peter Haynes [Opens in a new window] ,
Francis Auclair Open the ORCID record for Francis Auclair [Opens in a new window]  and
Cyril Nguyen Open the ORCID record for Cyril Nguyen [Opens in a new window]
Jared Penney*
Affiliation:
LEGOS, Université de Toulouse, CNES, CNRS, IRD, UPS, Toulouse31400, France
Yves Morel
Affiliation:
LEGOS, Université de Toulouse, CNES, CNRS, IRD, UPS, Toulouse31400, France
Peter Haynes
Affiliation:
Department of Applied Mathematics and Theoretical Physics, University of Cambridge, CambridgeCB3 0WA, UK
Francis Auclair
Affiliation:
Laboratoire d'Aérologie, Université de Toulouse, CNRS, UPS, Toulouse31400, France
Cyril Nguyen
Affiliation:
Laboratoire d'Aérologie, Université de Toulouse, CNRS, UPS, Toulouse31400, France
*
†Email address for correspondence: jared.penney@legos.obs-mip.fr
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Abstract

This paper considers the diapycnal transport of passive tracers during a Kelvin–Helmholtz mixing event. Numerical simulations of a traditional Kelvin–Helmholtz (KH) configuration of a stratified shear flow are extended to include layers of passive tracer at different locations relative to the shear layer. The evolution of the tracers during the simulation is followed and is analysed using different theoretical approaches. One is to consider the evolution via the distribution in density–tracer space which clearly reveals how the tracers are redistributed across isopycnals by the mixing driven by the growing and saturating KH billow. The shape of the distribution places constraints on the redistribution of the tracer and, for this problem of symmetrically stratified shear, it is shown that the distribution typically tends to a compact form, with significant regions that are nearly linear. The redistribution across isopycnals is also considered via a diffusion equation for the tracer relative to coordinates based on the geometry of density surfaces. The equation is a generalisation of an equation previously derived for transport of density in these coordinates and includes an extra eddy term that arises because there is variation of the tracer along density surfaces. Under certain circumstances and at later stages of the flow, the eddy term can be neglected, and the evolution of the mean tracer profile can be adequately represented using a simple diffusion equation where diffusivity is defined as the effective diffusivity of density, scaled by the molecular diffusion of the tracer.

JFM classification

Turbulent Flows: Stratified turbulence
Type
JFM Papers
Information
Journal of Fluid Mechanics , Volume 900 , 10 October 2020 , A26
Copyright
© The Author(s), 2020. Published by Cambridge University Press

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References

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