We provide benchmark comparisons of two finite element (FE) mantle convection codes, CITCOM and CONMAN, against analytic solutions for Stokes' flow for strongly varying viscosity in the horizontal and vertical directions. The two codes use a similar FE formulation but different methods for solving the resulting equations. They both obtain accurate velocity, pressure and surface topography for viscosity structures which vary rapidly over a short distance, or discontinuously. The benchmarks help determine how many elements are needed to resolve a region of, for example, a convection simulation with high viscosity gradients. The overall accuracy does not depend on the global viscosity variation but on the gradients within individual elements. ...
In this dissertation we describe the design, implementation, and use of a two-dimensional, second-or...
peer-reviewedMotivated by convection of planetary mantles, we consider a mathematical model for Rayl...
A mantle convection model consisting of the stationary Stokes equations and a time dependent convect...
Geodynamical simulations over the past decades have widely been built on quadrilateral and hexahedra...
A Finite Element Method for solving the convection problem in a fluid with position-dependent Newton...
Key words Incompressible Stokes equations, variable viscosity, finite element error analysis, depend...
Finite element error estimates are derived for the incompressible Stokes equations with variable vis...
A mantle convection model consisting of the stationary Stokes equations and a time-dependent convect...
Geodynamic modeling is often related with challenging computations involving solution of the Stokes ...
Accurate determination of surface normal stresses from numerical modeling of mantle convection is cr...
Numerical solutions to thermal convection flow problems are vital to many scientific and engineerin...
Convection in the Earth's mantle is a complicated phenomenon that causes various tectonic activitie...
Numerical simulations of thermal convection in the Earth’s mantle often employ a pseudoplastic rheol...
The performance of several numerical schemes for discretizing convection-dominated convection–diffus...
We investigate the optimal accuracy of the streamline diffusion finite element method applied to con...
In this dissertation we describe the design, implementation, and use of a two-dimensional, second-or...
peer-reviewedMotivated by convection of planetary mantles, we consider a mathematical model for Rayl...
A mantle convection model consisting of the stationary Stokes equations and a time dependent convect...
Geodynamical simulations over the past decades have widely been built on quadrilateral and hexahedra...
A Finite Element Method for solving the convection problem in a fluid with position-dependent Newton...
Key words Incompressible Stokes equations, variable viscosity, finite element error analysis, depend...
Finite element error estimates are derived for the incompressible Stokes equations with variable vis...
A mantle convection model consisting of the stationary Stokes equations and a time-dependent convect...
Geodynamic modeling is often related with challenging computations involving solution of the Stokes ...
Accurate determination of surface normal stresses from numerical modeling of mantle convection is cr...
Numerical solutions to thermal convection flow problems are vital to many scientific and engineerin...
Convection in the Earth's mantle is a complicated phenomenon that causes various tectonic activitie...
Numerical simulations of thermal convection in the Earth’s mantle often employ a pseudoplastic rheol...
The performance of several numerical schemes for discretizing convection-dominated convection–diffus...
We investigate the optimal accuracy of the streamline diffusion finite element method applied to con...
In this dissertation we describe the design, implementation, and use of a two-dimensional, second-or...
peer-reviewedMotivated by convection of planetary mantles, we consider a mathematical model for Rayl...
A mantle convection model consisting of the stationary Stokes equations and a time dependent convect...