Backus problem in geophysics: a resolution near the dipole in fractional Sobolev spaces
Toru Kan, Rolando Magnanini, Michiaki Onodera

TL;DR
This paper addresses the complex problem of reconstructing Earth's magnetic potential from surface measurements, focusing on the linearized dipole case using fractional Sobolev spaces to establish existence and uniqueness of solutions.
Contribution
It provides the first local existence and uniqueness results for the linearized geomagnetic Backus problem in fractional Sobolev spaces, specifically near a dipole in axially symmetric cases.
Findings
Existence of harmonic solutions near a dipole in fractional Sobolev spaces.
Solutions are constructed as series of spherical harmonics.
Unique solutions are obtained by prescribing the potential's average on the equatorial circle.
Abstract
We consider Backus's problem in geophysics. This consists in reconstructing a harmonic potential outside the Earth when the intensity of the related field is measured on the Earth's surface. Thus, the boundary condition is (severely) nonlinear. The gravitational case is quite understood. It consists in the local resolution near a monopole, i.e. the potential generated by a point mass. In this paper, we consider the geomagnetic case. This consists in linearizing the field's intensity near the so-called dipole, a harmonic function which models the solenoidal potential of a magnet. The problem is quite difficult, because the resolving operator related to the linearized problem is generally unbounded. Indeed, existence results for Backus's problem in this framework are not present in the literature. In this work, we locally solve the geomagnetic version of Backus's problem in the axially…
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Taxonomy
TopicsNumerical methods in inverse problems · Numerical methods in engineering · Differential Equations and Boundary Problems
