Abstract We report the current status of our numerical simulation code named “ACuTEMan ” for large-scale mantle convection problems on the Earth Simulator. The ACuTEMan code comes out from a newly-devel-oped “ACuTE ” algorithm, which solves the flow field of mantle convection in combination with the multi-grid method. This algorithm iteratively solves the steady-state equations for conservation of mass and momentum for highly viscous and incompressible fluids, and is proved to be suitable for mantle convection problems with excellent vector and parallel capability. In addition, a careful adaptation of the multigrid proce-dure enabled us to obtain a moderate parallel efficiency using up to 64 processor nodes of the Earth Simulator. In this p...
Solver coupling can extend the capability of existing modeling software and provide a new venue to a...
Computational models yield inaccurate results if the underlying numerical grid fails to provide the ...
The Earth mantle convects on a global scale, coupling the stress field at every point to every other...
The long-term motion of the Earth's mantle is of considerable interest to geologists and geodynamist...
Modelling of geodynamic processes like mantle or core convection has strongly improved over the last...
Convection of the 3000 km thick rocky mantle and the liquid iron core below it are the two most impo...
This is a poster describing three algorithms or Scientific Software Elements (SSEs) for computing / ...
A three-dimensional finite-element method is used to investigate thermal convection in the earth's m...
Abstract—Mantle convection is the principal control on the thermal and geological evolution of the E...
Thermal convection is a universal phenomenon in nature and has many geophysical applications such as...
A method for incorporating multi-resolution capabilities within pre-existing global 3-D spherical ma...
In this dissertation we describe the design, implementation, and use of a two-dimensional, second-or...
A new generation, parallel adaptive-mesh mantle convection code, Rhea, is described and benchmarked....
The thermal convection of rock in Earth's mantle and associated plate tectonics are modeled by nonli...
Center (SESG/ESC) is conducting numerical simulations of mantle convection in a three-dimensional re...
Solver coupling can extend the capability of existing modeling software and provide a new venue to a...
Computational models yield inaccurate results if the underlying numerical grid fails to provide the ...
The Earth mantle convects on a global scale, coupling the stress field at every point to every other...
The long-term motion of the Earth's mantle is of considerable interest to geologists and geodynamist...
Modelling of geodynamic processes like mantle or core convection has strongly improved over the last...
Convection of the 3000 km thick rocky mantle and the liquid iron core below it are the two most impo...
This is a poster describing three algorithms or Scientific Software Elements (SSEs) for computing / ...
A three-dimensional finite-element method is used to investigate thermal convection in the earth's m...
Abstract—Mantle convection is the principal control on the thermal and geological evolution of the E...
Thermal convection is a universal phenomenon in nature and has many geophysical applications such as...
A method for incorporating multi-resolution capabilities within pre-existing global 3-D spherical ma...
In this dissertation we describe the design, implementation, and use of a two-dimensional, second-or...
A new generation, parallel adaptive-mesh mantle convection code, Rhea, is described and benchmarked....
The thermal convection of rock in Earth's mantle and associated plate tectonics are modeled by nonli...
Center (SESG/ESC) is conducting numerical simulations of mantle convection in a three-dimensional re...
Solver coupling can extend the capability of existing modeling software and provide a new venue to a...
Computational models yield inaccurate results if the underlying numerical grid fails to provide the ...
The Earth mantle convects on a global scale, coupling the stress field at every point to every other...