A novel approach to the construction of three-dimensional grids in spherical geometries is described. The grids are based on a range of underlying regular polyhedra. The faces of the polyhedra are arranged into a number of diamonds in the latitudinal and longitudinal directions to facilitate the creation of a structured mesh. Each polyhedron is completely characterized in terms of the arrangement of diamonds. The approach is shown to be very flexible in terms of the meshes that can be generated. It also aids comparisons between the grids used in many mantle convection studies. A spectral element discretization of Poisson's equation is performed to demonstrate the efficacy of the grid generation technique. Rapidly convergent approximations a...
This article proposes a new grid system for the sphere, which consists of three orthogonal and almos...
This article proposes a new grid system for the sphere, which consists of three orthogonal and almos...
Convection of the 3000 km thick rocky mantle and the liquid iron core below it are the two most impo...
A novel approach to the construction of three-dimensional grids in spherical geometries is described...
A method for incorporating multi-resolution capabilities within pre-existing global 3-D spherical ma...
This paper presents a new method to generate a three-dimensional spherical grid using natural neighb...
An arbitrary finite-volume approach is developed for discretising partial differential equations gov...
Computational models yield inaccurate results if the underlying numerical grid fails to provide the ...
An algorithm for the generation of non-uniform, locally orthogonal staggered unstructured spheroidal...
One of the most important advances needed in global climate models is the development of atmospheric...
A new method for generating a numerical grid on a spherical surface is presented. This method allows...
An algorithm for the generation of non-uniform, locally orthogonal staggered unstructured spheroidal...
Computational models of mantle convection must accurately represent curved boundaries and the associ...
AbstractA simple geometric condition that defines the class of classical (stereographic, conic and c...
The article of record as published may be located at http://dx.doi.org/10.1006/jcph.1997.5771Lagrang...
This article proposes a new grid system for the sphere, which consists of three orthogonal and almos...
This article proposes a new grid system for the sphere, which consists of three orthogonal and almos...
Convection of the 3000 km thick rocky mantle and the liquid iron core below it are the two most impo...
A novel approach to the construction of three-dimensional grids in spherical geometries is described...
A method for incorporating multi-resolution capabilities within pre-existing global 3-D spherical ma...
This paper presents a new method to generate a three-dimensional spherical grid using natural neighb...
An arbitrary finite-volume approach is developed for discretising partial differential equations gov...
Computational models yield inaccurate results if the underlying numerical grid fails to provide the ...
An algorithm for the generation of non-uniform, locally orthogonal staggered unstructured spheroidal...
One of the most important advances needed in global climate models is the development of atmospheric...
A new method for generating a numerical grid on a spherical surface is presented. This method allows...
An algorithm for the generation of non-uniform, locally orthogonal staggered unstructured spheroidal...
Computational models of mantle convection must accurately represent curved boundaries and the associ...
AbstractA simple geometric condition that defines the class of classical (stereographic, conic and c...
The article of record as published may be located at http://dx.doi.org/10.1006/jcph.1997.5771Lagrang...
This article proposes a new grid system for the sphere, which consists of three orthogonal and almos...
This article proposes a new grid system for the sphere, which consists of three orthogonal and almos...
Convection of the 3000 km thick rocky mantle and the liquid iron core below it are the two most impo...