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On Instability Properties of the Fractional Calder\'{o}n Problem
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abstract
We prove exponential instability properties for the fractional Calder\'on problem and the conductivity formulation of the fractional Calder\'on problem in the regime of fractional powers $s\in (0,1)$. We particularly focus on two settings: First, we discuss instability properties in general domain geometries with scaling critical $L^{\frac{n}{2s}}$ potentials and constant background metrics. Secondly, we investigate instability properties in general geometries with $L^{\frac{n}{2s}}$ potentials and low regularity, variable coefficient, possibly anisotropic background metrics. In both settings we make use of the methods introduced in \cite{KRS21} and we deduce strong compression estimates for the forward problem. In the first setting this is based on analytic smoothing estimates for a suitable comparison operator while in the second setting involving low regularity metrics this is based on an iterated compression gain. We thus generalize the results from \cite{RS18} to generic geometries and variable coefficients and further also discuss the setting of fractional conductivity equations. In particular, this proves that the logarithmic stability estimates for the fractional Calder\'on problem from \cite{RS20} are optimal.
Forward citations
Cited by 3 Pith papers
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Geometrical optics for the fractional Helmholtz equation and applications to inverse problems
Fractional Helmholtz operators admit high-frequency geometrical optics solutions, and for s≥1/2 these give Hölder stable recovery of the potential from multi-frequency boundary Cauchy data.
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Fractional anisotropic Calder\'on problem with external data
Exterior Dirichlet-to-Neumann data for fractional Laplace-Beltrami operators determine a Euclidean-asymptotic Riemannian metric up to a diffeomorphism fixing the exterior.
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A Calder\'on type inverse problem for the active scalar equations with fractional dissipation
If two active scalar equations with fractional dissipation produce the same observations on a small open set, their nonlocal drift operators must agree on the whole exterior, according to the paper's main theorem.
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