Abstract
Forced advection of passive scalar by a smooth -dimensional incompressible velocity in the presence of a linear damping is studied. Acting separately advection and dumping do not lead to an essential intermittency of the steady scalar statistics, while being mixed together produce a very strong non-Gaussianity in the convective range: -th (positive) moment of the absolute value of scalar difference, is proportional to , , where measures the rate of the damping in the units of the stretching rate. Probability density function (PDF) of the scalar difference is also found.
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