Large-scale effects on meso-scale modeling for scalar transport
arXiv:nlin/0507053 · doi:10.1016/j.physd.2006.07.007
Abstract
The transport of scalar quantities passively advected by velocity fields with a small-scale component can be modeled at meso-scale level by means of an effective drift and an effective diffusivity, which can be determined by means of multiple-scale techniques. We show that the presence of a weak large-scale flow induces interesting effects on the meso-scale scalar transport. In particular, it gives rise to non-isotropic and non-homogeneous corrections to the meso-scale drift and diffusivity. We discuss an approximation that allows us to retain the second-order effects caused by the large-scale flow. This provides a rather accurate meso-scale modeling for both asymptotic and pre-asymptotic scalar transport properties. Numerical simulations in model flows are used to illustrate the importance of such large-scale effects.
19 pages, 8 figures
References in corpus (5)
Cited by in corpus (5)
- Eddy diffusivities of inertial particles under gravity
- Generalization of Taylor's formula to particles of arbitrary inertia
- Combined role of molecular diffusion, mean streaming and helicity in the eddy diffusivity of short-correlated random flows
- Eddy diffusivity of quasi-neutrally-buoyant inertial particles
- Settling velocity of quasi-neutrally-buoyant inertial particles