A convergence result for an iterative method for the equations of a stationary quasi-newtonian flow with temperature dependent viscosity
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S. Wardi (1998)
ESAIM: Mathematical Modelling and Numerical Analysis - Modélisation Mathématique et Analyse Numérique
Jaroslav Haslinger, Josef Málek, Jan Stebel (2005)
Control and Cybernetics
Jordan, P.M. (2005)
Mathematical Problems in Engineering
Weizhu Bao, John W. Barrett (1998)
ESAIM: Mathematical Modelling and Numerical Analysis - Modélisation Mathématique et Analyse Numérique
Massoudi, Mehrdad, Antaki, James F. (2008)
Mathematical Problems in Engineering
Jacques Baranger, Khalid Najib (1990/1991)
Numerische Mathematik
M. Bulíček, Josef Málek, Kumbakonam R. Rajagopal (2009)
Czechoslovak Mathematical Journal
Over a large range of the pressure, one cannot ignore the fact that the viscosity grows significantly (even exponentially) with increasing pressure. This paper concerns long-time and large-data existence results for a generalization of the Navier-Stokes fluid whose viscosity depends on the shear rate and the pressure. The novelty of this result stems from the fact that we allow the viscosity to be an unbounded function of pressure as it becomes infinite. In order to include a large class of viscosities...
Wilfried Weinelt (1984)
Banach Center Publications
Roland Glowinski, Jacques Rappaz (2003)
ESAIM: Mathematical Modelling and Numerical Analysis - Modélisation Mathématique et Analyse Numérique
The main goal of this article is to establish a priori and a posteriori error estimates for the numerical approximation of some non linear elliptic problems arising in glaciology. The stationary motion of a glacier is given by a non-newtonian fluid flow model which becomes, in a first two-dimensional approximation, the so-called infinite parallel sided slab model. The approximation of this model is made by a finite element method with piecewise polynomial functions of degree 1. Numerical results...
Roland Glowinski, Jacques Rappaz (2010)
ESAIM: Mathematical Modelling and Numerical Analysis
The main goal of this article is to establish a priori and a posteriori error estimates for the numerical approximation of some non linear elliptic problems arising in glaciology. The stationary motion of a glacier is given by a non-Newtonian fluid flow model which becomes, in a first two-dimensional approximation, the so-called infinite parallel sided slab model. The approximation of this model is made by a finite element method with piecewise polynomial functions of degree 1. Numerical results...
Boughanim, Fouad, Boukrouche, Mahdi, Smaoui, Hassan (2004)
Electronic Journal of Differential Equations (EJDE) [electronic only]
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