Chrysoula Tsogka

Prof. Chrysoula Tsogka

University of California, Merced, Merced, California, USA
+1
orcid

Research Focus & Metrics

Academic Career Length

30Years (1997-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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1 January 2001 in Geophysics
Verified
Journal Article
Closed access
FCFrancis Collino
Francis Collino
CTChrysoula Tsogka
Chrysoula Tsogka
We present and analyze a perfectly matched, absorbing layer model for the velocity-stress formulation of elastodynamics. The principal idea of this method consists of introducing an absorbing layer in which we decompose each component of the unknown into two auxiliary components: a component orthogonal to the boundary and a component parallel to it. A system of equations governing these new unknowns then is constructed. A damping term finally is introduced for the component orthogonal to the boundary. This layer model has the property of generating no reflection at the interface between the free medium and the artificial absorbing medium. In practice, both the boundary condition introduced at the outer boundary of the layer and the dispersion resulting from the numerical scheme produce a small reflection which can be controlled even with very thin layers. As we will show with several experiments, this model gives very satisfactory results; namely, the reflection coefficient, even in the case of heterogeneous, anisotropic media, is about 1% for a layer thickness of five space discretization steps.

31 July 2002 in Inverse Problems
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Journal Article
Closed access
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LBLiliana Borcea
Liliana Borcea
GPGeorge Papanicolaou
George Papanicolaou
CTChrysoula Tsogka
Chrysoula Tsogka
JBJames Berryman
James Berryman

1 January 2000 in SIAM Journal on Numerical Analysis
Verified
Journal Article
Open access
EBE. Bécache
E. Bécache
PJP. Joly
P. Joly
CTChrysoula Tsogka
Chrysoula Tsogka
We construct and analyze a new family of rectangular (two-dimensional) or cubic (three-dimensional) mixed finite elements for the approximation of the acoustic wave equations. The main advantage of this element is that it permits us to obtain through mass lumping an explicit scheme even in an anisotropic medium. Nonclassical error estimates are given for this new element.

12 November 2003 in Inverse Problems
Verified
Journal Article
Closed access
LBLiliana Borcea
Liliana Borcea
GPGeorge Papanicolaou
George Papanicolaou
CTChrysoula Tsogka
Chrysoula Tsogka

25 July 2005 in Inverse Problems
Verified
Journal Article
Closed access
LBLiliana Borcea
Liliana Borcea
GPGeorge Papanicolaou
George Papanicolaou
CTChrysoula Tsogka
Chrysoula Tsogka

18 July 2006 in Inverse Problems
Verified
Journal Article
Closed access
LBLiliana Borcea
Liliana Borcea
GPGeorge Papanicolaou
George Papanicolaou
CTChrysoula Tsogka
Chrysoula Tsogka