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We study the stability in the inverse problem of determining the time dependent zeroth-order coefficient arising in the wave equation, from boundary observations. We derive, in dimension , a log-type stability estimate in the determination of from the Dirichlet-to-Neumann map, in a subset of our domain assuming that it is known outside this subset. Moreover, we prove that we can extend this result to the determination of in a larger region, and then in the whole domain provided that we have much more data.

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