Abstract. The manufactured solution technique is used for the verification of computational models in many fields. In this paper, we construct manufactured solutions for the three-dimensional, isothermal, nonlinear Stokes model for flows in glaciers and ice sheets. The solution construction proce-dure starts with kinematic boundary conditions and is mainly based on the solution of a first-order partial differential equa-tion for the ice velocity that satisfies the incompressibility condition. The manufactured solutions depend on the geom-etry of the ice sheet, basal sliding parameters, and ice soft-ness. Initial conditions are taken from the periodic geometry of a standard problem of the ISMIP-HOM benchmark tests. The upper surface is alter...
In this chapter, we analyze and approximate a nonlinear stationary Stokes problem that describes the...
Ice sheets have strong influence on the climate system. Numerical simulation provides a mathematical...
Abstract: In this work we consider a 3D isothermal mathematical model for ice sheets flows over a ho...
The numerical modeling of glacier and ice sheet evolution is a subject of growing interest, in part ...
Abstract. A three-dimensional full-Stokes computational model is considered for deter-mining the dyn...
A three-dimensional full-Stokes computational model is considered for determining the dynamics, temp...
The increase in computational power in the last 20 years has made it feasible to solve the full Stok...
Abstract. The numerical modeling of glacier and ice sheet evolution is a subject of grow-ing interes...
The Fourth IPCC Assessment Report concluded that ice sheet flow models, in their current state, were...
Ice sheets, such as the Greenland Ice Sheet or Antarctic Ice Sheet, have a fundamental impact on lan...
This paper describes a new parallel, scalable and robust finite element based solver for the first-o...
This research involves a few First-Order System Least Squares (FOSLS) formulations of a nonlinear-St...
Abstract. Motivated by the need for efficient and accurate simulation of the dynamics of the polar i...
Ice flow, forced by gravity is governed by the Full Stokes (FS) equations, which are computationally...
A computational analysis of the accuracy of different approximations to the Stokes equations for mom...
In this chapter, we analyze and approximate a nonlinear stationary Stokes problem that describes the...
Ice sheets have strong influence on the climate system. Numerical simulation provides a mathematical...
Abstract: In this work we consider a 3D isothermal mathematical model for ice sheets flows over a ho...
The numerical modeling of glacier and ice sheet evolution is a subject of growing interest, in part ...
Abstract. A three-dimensional full-Stokes computational model is considered for deter-mining the dyn...
A three-dimensional full-Stokes computational model is considered for determining the dynamics, temp...
The increase in computational power in the last 20 years has made it feasible to solve the full Stok...
Abstract. The numerical modeling of glacier and ice sheet evolution is a subject of grow-ing interes...
The Fourth IPCC Assessment Report concluded that ice sheet flow models, in their current state, were...
Ice sheets, such as the Greenland Ice Sheet or Antarctic Ice Sheet, have a fundamental impact on lan...
This paper describes a new parallel, scalable and robust finite element based solver for the first-o...
This research involves a few First-Order System Least Squares (FOSLS) formulations of a nonlinear-St...
Abstract. Motivated by the need for efficient and accurate simulation of the dynamics of the polar i...
Ice flow, forced by gravity is governed by the Full Stokes (FS) equations, which are computationally...
A computational analysis of the accuracy of different approximations to the Stokes equations for mom...
In this chapter, we analyze and approximate a nonlinear stationary Stokes problem that describes the...
Ice sheets have strong influence on the climate system. Numerical simulation provides a mathematical...
Abstract: In this work we consider a 3D isothermal mathematical model for ice sheets flows over a ho...