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The Obukhov–Corrsin spectrum predicts the distribution of Fourier mass for a passive scalar field advected by a “turbulent” velocity field with spatial regularity for and subject to a time-stationary forcing. We prove the Obukhov–Corrsin spectrum holds after summing over geometric annuli in Fourier space – up to logarithmic corrections – as a consequence of a sharp anomalous regularization result. We then prove this anomalous regularization for a broad class of Kraichnan-type models. The proof of anomalous regularization relies on a Fourier space energy equality and a weighted lattice Poincaré inequality.

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