An isotropic passive scalar field T advected by a rapidly-varying velocity
field is studied. The tail of the probability distribution P(θ,r) for
the difference θ in T across an inertial-range distance r is found
to be Gaussian. Scaling exponents of moments of θ increase as n
or faster at large order n, if a mean dissipation conditioned on θ is
a nondecreasing function of ∣θ∣. The P(θ,r) computed numerically
under the so-called linear ansatz is found to be realizable. Some classes of
gentle modifications of the linear ansatz are not realizable.Comment: Substantially revised to conform with published version. Revtex (4
pages) with 2 postscript figures. Send email to [email protected]