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Dive into the research topics where Heinz-Otto Kreiss is active.

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Featured researches published by Heinz-Otto Kreiss.


Mathematics of Computation | 1972

Stability theory of difference approximations for mixed initial boundary value problems. II

Bertil Gustafsson; Heinz-Otto Kreiss; Arne Sundström

Stability theory of difference approximations for mixed initial boundary value problems. II


Bit Numerical Mathematics | 1962

Über Die Stabilitätsdefinition Für Differenzengleichungen Die Partielle Differentialgleichungen Approximieren

Heinz-Otto Kreiss

For difference equations with constant coefficients necessary and sufficient algebraic stability conditions are given for the stability definitions used by G. Forsythe and W. Wasow (A) and P. D. Lax and R. D. Richtmyer (B). The application of these conditions for difference equations with variable coefficients is considered and it is shown that the stability condition of definitionA is not sufficient for stability. The same is true with respect to the definitionB if the difference equations are not parabolic and do not approximate first order systems. Therefore another stability definition is proposed and a number of properties are discussed.


SIAM Journal on Numerical Analysis | 1977

Stability of the Fourier method

Heinz-Otto Kreiss; Joseph Oliger

In this paper we develop a stability theory for the Fourier (or pseudo-spectral) method for linear hyperbolic and parabolic partial differential equations with variable coefficients.


Numerische Mathematik | 1974

Difference approximations for singular perturbations of systems of ordinary differential equations

Leif R. Abrahamsson; Herbert B. Keller; Heinz-Otto Kreiss

SummaryWe consider difference methods for the solution of singular perturbations of boundary value problems. The solutions are smooth except in boundary layers of thickness ε|logε|, 0<ε≪1. Various difference schemes with a uniform stepsizeh are considered. In practice,h is usually much larger than the boundary layer regions. Then the difference methods must be choosen with care. It is shown that only approximations of low order accuracy can be used. However, one can increase the accuracy by a Richardson procedure. Asymptotic expansions in powers ofh and ε are given for the solutions of the proposed methods.


Advances in Applied Mathematics | 1991

Convergence of the solutions of the compressible to the solutions of the incompressible Navier-Stokes equations

Heinz-Otto Kreiss; Jens Lorenz; M.J Naughton

We study the slightly compressible Navier-Stokes equations. We first consider the Cauchy problem, periodic in space. Under appropriate assumptions on the initial data, the solution of the compressible equations consists-to first order-of a solution of the incompressible equations plus a function which is highly oscillatory in time. We show that the highly oscillatory part (the sound waves) can be described by wave equations, at least locally in time. We also show that the bounded derivative principle is valid; i.e., the highly oscillatory part can be suppressed by initialization. Besides the Cauchy problem, we also consider an initial-boundary value problem. At the inflow boundary, the viscous term in the Navier-Stokes equations is important. We consider the case where the compressible pressure is prescribed at inflow. In general, one obtains a boundary layer in the pressure; in the velocities a boundary layer is not present to first approximation.


SIAM Journal on Numerical Analysis | 2007

Stable Difference Approximations for the Elastic Wave Equation in Second Order Formulation

Stefan Nilsson; N. Anders Petersson; Björn Sjögreen; Heinz-Otto Kreiss

We consider the three-dimensional elastic wave equation for an isotropic heterogeneous material subject to a stress-free boundary condition. Building on our recently developed theory for difference methods for second order hyperbolic systems [H.-O. Kreiss, N. A. Petersson, J. Ystrom, SIAM J. Numer. Anal., 40 (2002), pp. 1940-1967], we develop an explicit, second order accurate technique which is stable for all ratios of longitudinal over transverse phase velocities. The spatial discretization is self-adjoint, and the stability is obtained through an energy estimate. Seismic events are often modeled using singular source terms, and we devise a technique to place sources independently of the grid while retaining second order accuracy away from the source. Several numerical examples are given.


SIAM Journal on Numerical Analysis | 1978

Difference Methods for Stiff Ordinary Differential Equations

Heinz-Otto Kreiss

Consider the initial value problem for a first order system of stiff ordinary differential equations. The smoothness properties of its solutions are investigated and a general theory for difference...


SIAM Journal on Scientific Computing | 2005

A Second Order Accurate Embedded Boundary Method for the Wave Equation with Dirichlet Data

Heinz-Otto Kreiss; N. Anders Petersson

The accuracy of Cartesian embedded boundary methods for the second order wave equation in general two-dimensional domains subject to Dirichlet boundary conditions is analyzed. Based on the analysis, we develop a numerical method where both the solution and its gradient are second order accurate. We avoid the small-cell stiffness problem without sacrificing the second order accuracy by adding a small artificial term to the Dirichlet boundary condition. Long-time stability of the method is obtained by adding a small fourth order dissipative term. Several numerical examples are provided to demonstrate the accuracy and stability of the method. The method is also used to solve the two-dimensional TM


SIAM Journal on Numerical Analysis | 2004

Difference Approximations of the Neumann Problem for the Second Order Wave Equation

Heinz-Otto Kreiss; N. Anders Petersson; Jacob Yström

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SIAM Journal on Numerical Analysis | 1986

Numerical methods for stiff two-point boundary value problems

Heinz-Otto Kreiss; Nancy Nichols; David L. Brown

problem for Maxwells equations posed as a second order wave equation for the electric field coupled to ordinary differential equations for the magnetic field.

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Jens Lorenz

University of New Mexico

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Joseph Oliger

National Center for Atmospheric Research

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N. Anders Petersson

Lawrence Livermore National Laboratory

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Jacob Yström

Royal Institute of Technology

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Omar E. Ortiz

National University of Cordoba

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