The aim of this paper is to study a nonlinear stationary Stokes problem with mixed boundary conditions that describes the ice velocity and pressure fields of grounded glaciers under Glen's flow law. Using convex analysis arguments, we prove the existence and the uniqueness of a weak solution. A finite element method is applied with approximation spaces that satisfy the inf-sup condition, and a priori error estimates are established by using a quasinorm technique. Several algorithms (including Newton's method) are proposed to solve the nonlinearity of the Stokes problem and are proved to be convergent. Our results are supported by numerical convergence studies
The increase in computational power in the last 20 years has made it feasible to solve the full Stok...
A computational analysis of the accuracy of different approximations to the Stokes equations for mom...
A numerical method for the simulation of the motion of a glacier in two and three dimensions is pres...
In this chapter, we analyze and approximate a nonlinear stationary Stokes problem that describes the...
Abstract. Motivated by the need for efficient and accurate simulation of the dynamics of the polar i...
Abstract. The main goal of this article is to establish a priori and a posteriori error estimates fo...
In glacier dynamics – i.e. the field of research concerning the movement of ice – intricate mathemat...
The numerical modeling of glacier and ice sheet evolution is a subject of growing interest, in part ...
The main goal of this article is to establish a priori and a posteriori error estimates for the nu...
Abstract. The numerical modeling of glacier and ice sheet evolution is a subject of grow-ing interes...
This research involves a few First-Order System Least Squares (FOSLS) formulations of a nonlinear-St...
Viscous contact problems describe the time evolution of fluid flows in contact with a surface from w...
Stokes variational inequalities arise in the formulation of glaciological problems involving contact...
The computation of glacier movements leads to a system of nonlinear partial differential equations. ...
A stationary problem of the non-Newtonian fluid dynamics is applied to the modeling of an alpine gla...
The increase in computational power in the last 20 years has made it feasible to solve the full Stok...
A computational analysis of the accuracy of different approximations to the Stokes equations for mom...
A numerical method for the simulation of the motion of a glacier in two and three dimensions is pres...
In this chapter, we analyze and approximate a nonlinear stationary Stokes problem that describes the...
Abstract. Motivated by the need for efficient and accurate simulation of the dynamics of the polar i...
Abstract. The main goal of this article is to establish a priori and a posteriori error estimates fo...
In glacier dynamics – i.e. the field of research concerning the movement of ice – intricate mathemat...
The numerical modeling of glacier and ice sheet evolution is a subject of growing interest, in part ...
The main goal of this article is to establish a priori and a posteriori error estimates for the nu...
Abstract. The numerical modeling of glacier and ice sheet evolution is a subject of grow-ing interes...
This research involves a few First-Order System Least Squares (FOSLS) formulations of a nonlinear-St...
Viscous contact problems describe the time evolution of fluid flows in contact with a surface from w...
Stokes variational inequalities arise in the formulation of glaciological problems involving contact...
The computation of glacier movements leads to a system of nonlinear partial differential equations. ...
A stationary problem of the non-Newtonian fluid dynamics is applied to the modeling of an alpine gla...
The increase in computational power in the last 20 years has made it feasible to solve the full Stok...
A computational analysis of the accuracy of different approximations to the Stokes equations for mom...
A numerical method for the simulation of the motion of a glacier in two and three dimensions is pres...