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An isotropic passive scalar field advected by a rapidly-varying velocity field is studied. The tail of the probability distribution for the difference in across an inertial-range distance is found to be Gaussian. Scaling exponents of moments of increase as or faster at large order , if a mean dissipation conditioned on is a nondecreasing function of . The 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.

生成讲解博客的中文版本

生成AI智能校验的中文版本