Abstract
A systematic method is outlined for constructing workable approximations to the joint probability distribution scrP(ψ,ξ) of amplitude ψ and spatial gradient ξ of an active or passive scalar field that is advected by a prescribed isotropically distributed stochastic velocity field and subjected to molecular diffusion. scrP(ψ,ξ) is sampled along fluid-element paths, and closure is obtained by taking a multivariate-Gaussian reference field (x) and distorting it locally in x space so that it exhibits the current scrP(pxi,ξ).
- Received 7 August 1989
DOI:https://doi.org/10.1103/PhysRevLett.63.2657
©1989 American Physical Society