For with an independent equiprobable drift , the likelihood ratio between the two drifts is . Multiplying the normal distribution densities of successive increments proves this ratio for every observation partition; continuity then gives the full observed-path posterior. The Bayes' theorem gives . Thus the observed drift is . The process is an observed-filtration martingale with quadratic variation , so the Lévy characterization of Brownian motion makes it a Brownian motion. The observed state is a scaled diffusion with hyperbolic tangent drift.
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