Rigidity in the Lorentzian Calderón problem with formally determined data

We study the Lorentzian Calderón problem, where the objective is to determine a globally hyperbolic Lorentzian metric up to a boundary fixing diffeomorphism from boundary measurements given by the hyperbolic Dirichlet-to-Neumann map. This problem is a wave equation analogue of the Calderón problem on Riemannian manifolds. We prove that if a globally hyperbolic metric agrees with the Minkowski metric outside a compact set and has the same hyperbolic Dirichlet-to-Neumann map as the Minkowski metric, then it must be the Minkowski metric up to diffeomorphism. In fact this follows from a stronger result that solves a formally determined inverse problem with a much smaller amount of measurements. To prove these results we introduce a new method for geometric hyperbolic inverse problems. The method is based on distorted plane wave solutions and on a combination of geometric, topological and unique continuation arguments.

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Publication Details

Journal
Communications of the American Mathematical Society
Published
2026-06-29
DOI
https://doi.org/10.1090/cams/73
Primary Topic
Numerical methods in inverse problems
Type
article
Field-Weighted Citation Impact
0.00

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article

Rigidity in the Lorentzian Calderón problem with formally determined data

Lauri Oksanen, Mikko Salo, Rakesh
Communications of the American Mathematical Society
Numerical methods in inverse problems
article

Rigidity in the Lorentzian Calderón problem with formally determined data

Lauri Oksanen, Mikko Salo, Rakesh
article en

Abstract

We study the Lorentzian Calderón problem, where the objective is to determine a globally hyperbolic Lorentzian metric up to a boundary fixing diffeomorphism from boundary measurements given by the hyperbolic Dirichlet-to-Neumann map. This problem is a wave equation analogue of the Calderón problem on Riemannian manifolds. We prove that if a globally hyperbolic metric agrees with the Minkowski metric outside a compact set and has the same hyperbolic Dirichlet-to-Neumann map as the Minkowski metric, then it must be the Minkowski metric up to diffeomorphism. In fact this follows from a stronger result that solves a formally determined inverse problem with a much smaller amount of measurements. To prove these results we introduce a new method for geometric hyperbolic inverse problems. The method is based on distorted plane wave solutions and on a combination of geometric, topological and unique continuation arguments.

Communications of the American Mathematical SocietyVol. 6(14)
National Science Foundation, Academy of Finland, European Research Council
Openalex Percentile: Top 4%
Numerical methods in inverse problems
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