|
|
Showing 1 - 5 of
5 matches in All Departments
The domain of inverse problems has experienced a rapid expansion,
driven by the increase in computing power and the progress in
numerical modeling. When I started working on this domain years
ago, I became somehow fr-
tratedtoseethatmyfriendsworkingonmodelingwhereproducingexistence,
uniqueness, and stability results for the solution of their
equations, but that I was most of the time limited, because of the
nonlinearity of the problem, to
provethatmyleastsquaresobjectivefunctionwasdi?erentiable....Butwith
my experience growing, I became convinced that, after the inverse
problem has been properly trimmed, the ?nal least squares problem,
the one solved on the computer, should be Quadratically
(Q)-wellposed, thatis, both we- posed and optimizable:
optimizability ensures that a global minimizer of the least squares
function can actually be found using e?cient local optimization
algorithms, and wellposedness that this minimizer is stable with
respect to perturbation of the data. But the vast majority of
inverse problems are nonlinear, and the clas- cal mathematical
tools available for their analysis fail to bring answers to these
crucial questions: for example, compactness will ensure existence,
but provides no uniqueness results, and brings no information on
the presence or absenceofparasiticlocalminimaorstationarypoints..
Inverse problems in wave propagation occur in geophysics, ocean acoustics, civil and environmental engineering, ultrasonic non-destructive testing, biomedical ultrasonics, radar, astrophysics, as well as other areas of science and technology. The papers in this volume cover these scientific and technical topics, together with fundamental mathematical investigations of the relation between waves and scatterers.
This book describes the state of the art in the field of modeling
and solving numerically inverse problems of wave propagation and
diffraction. It addresses mathematicians, physicists and engineers
as well. Applications in such fields as acoustics, optics, and
geophysics are emphasized. Of special interest are the
contributions to two and three dimensional problems without
reducing symmetries. Topics treated are the obstacle problem,
scattering by classical media, and scattering by distributed media.
Inverse problems in wave propagation occur in geophysics, ocean
acoustics, civil and environmental engineering, ultrasonic
non-destructive testing, biomedical ultrasonics, radar,
astrophysics, as well as other areas of science and technology. The
papers in this volume cover these scientific and technical topics,
together with fundamental mathematical investigations of the
relation between waves and scatterers.
The domain of inverse problems has experienced a rapid expansion,
driven by the increase in computing power and the progress in
numerical modeling. When I started working on this domain years
ago, I became somehow fr-
tratedtoseethatmyfriendsworkingonmodelingwhereproducingexistence,
uniqueness, and stability results for the solution of their
equations, but that I was most of the time limited, because of the
nonlinearity of the problem, to
provethatmyleastsquaresobjectivefunctionwasdi?erentiable....Butwith
my experience growing, I became convinced that, after the inverse
problem has been properly trimmed, the ?nal least squares problem,
the one solved on the computer, should be Quadratically
(Q)-wellposed, thatis, both we- posed and optimizable:
optimizability ensures that a global minimizer of the least squares
function can actually be found using e?cient local optimization
algorithms, and wellposedness that this minimizer is stable with
respect to perturbation of the data. But the vast majority of
inverse problems are nonlinear, and the clas- cal mathematical
tools available for their analysis fail to bring answers to these
crucial questions: for example, compactness will ensure existence,
but provides no uniqueness results, and brings no information on
the presence or absenceofparasiticlocalminimaorstationarypoints..
|
|