Layering and vertical transport in sheared double diffusive convection in the diffusive regime

TL;DR

This study investigates how shear influences layered structures and vertical scalar transport in double diffusive convection within the diffusive regime, revealing robust staircase formations and shear-modified flux ratios through simulations.

Contribution

It demonstrates the persistence of staircase structures under shear and quantifies the impact of shear on scalar fluxes and transport properties in double diffusive convection.

Findings

Staircase-like structures form spontaneously and are robust under shear.

Different initial perturbations lead to varied layered states with distinct fluxes.

Shear modifies the vertical scalar transport and flux ratios in the flow.

Abstract

A sequence of two and three-dimensional simulations is conducted for the double diffusive convection (DDC) flows in the diffusive regime subjected to an imposed shear. The flow is confined between two horizontal plates which are maintained at different constant temperature, salinity, and different velocity, thus setting up a shear across the flow. The lower plate is fixed at higher temperature and salinity, while the overall (unperturbed) density gradient is statically stable. For a wide range of control parameters, and for sufficiently strong perturbation of the conductive initial state, we find that staircase-like structures spontaneously develop, with relatively well-mixed layers separated by sharp interfaces of enhanced scalar gradient. Such staircases appear to be robust even in the presence of strong shear over very long times, although we typically observe early time coarsening of the number of observed layers. For the same set of control parameters, different asymptotic layered states, with markedly different vertical scalar fluxes, can arise for different initial perturbation structures. The imposed shear does significantly spatio-temporally modify the vertical transport of the various scalars. The flux ratio (i.e., the ratio between the density fluxes due to the total (convective and diffusive) salt flux and the total heat flux) is found, at steady state, to be essentially equal to the square root of the ratio of the salt diffusivity to the thermal diffusivity, consistently with the physical model originally proposed by Linden and Shirtcliffe (1978) and the variational arguments presented by Stern (1982) for unsheared double diffusive convection.