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Some generalizations in the mathematical developments of the theory of the geodetic overdetermined problems.

F. Sacerdote, F. Sansò (1990)

Revista Matemática de la Universidad Complutense de Madrid

Two particular cases of the overdetermined gravimetry-gradiometry problem are discussed: (i) the case of a latitude-dependant statistical weight for gradiometric data, corresponding to a data distribution coming from satellite polar orbits, (ii) the case of a volume distribution, instead of a surface distribution, for satellite gradiometric data. In both cases a discussion of numerical methods for solving the problem with realistic data is started; for case (i), an analytic solution is found under...

Some inverse and control problems for fluids

Enrique Fernández-Cara, Thierry Horsin, Henry Kasumba (2013)

Annales mathématiques Blaise Pascal

This paper deals with some inverse and control problems for the Navier-Stokes and related systems. We will focus on some particular aspects that have recently led to interesting (theoretical and numerical) results: geometric inverse problems, Eulerian and Lagrangian controllability and vortex reduction oriented to shape optimization.

Stability estimates for an inverse problem for the linear Boltzmann equation.

Rolci Cipolatti, Carlos M. Motta, Nilson C. Roberty (2006)

Revista Matemática Complutense

In this paper we consider the inverse problem of recovering the total extinction coefficient and the collision kernel for the time-dependent Boltzmann equation via boundary measurements. We obtain stability estimates for the extinction coefficient in terms of the albedo operator and also an identification result for the collision kernel.

Stability of the inverse problem in potential scattering at fixed energy

Plamen Stefanov (1990)

Annales de l'institut Fourier

We prove an estimate of the kind q 1 - q 2 L C ϕ ( A q 1 - A q 2 R , 3 / 2 - 1 / 2 ) , where A q i ( ω , θ ) , i = 1 , 2 is the scattering amplitude related to the compactly supported potential q i ( x ) at a fixed energy level k = const., ϕ ( t ) = ( - ln t ) - δ , 0 < δ < 1 and · R , 3 / 2 - 1 / 2 is a suitably defined norm.

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