On the Kraichnan Model of Passive Scalar Advection Near the Batchelor limit

Abstract

The third order correlation function of the scalar field advected by a Gaussian random velocity, with a spatial scaling exponent $2-\epsilon$, and in the presence of a mean gradient, is calculated perturbatively in $\epsilon <<1$. This expansion corresponds to the regime close to Batchelor's advection by linear diffeomorphisms. The scaling exponent is found to be equal to 1 in dimensions 2 and 3, up to corrections smaller than $\mathcal{O}(\epsilon )$, implying an anomalous scaling of the third order correlation function and the persistence of small scale anisotropy.