Implementation of an Atmosphere–Ocean General Circulation Model on the Expanded Spherical Cube
- 1 December 2004
- journal article
- Published by American Meteorological Society in Monthly Weather Review
- Vol. 132 (12), 2845-2863
- https://doi.org/10.1175/mwr2823.1
Abstract
A hydrodynamical kernel that drives both an atmospheric and oceanic general circulation model is implemented in general orthogonal curvilinear coordinates using the finite-volume method on the sphere. The finite-volume method naturally describes arbitrary grids, and use of the vector-invariant form of the momentum equations simplifies the generalization to arbitrary coordinates. Grids based on the expanded spherical cube of Rancic et al., which contain eight singular points, are used. At these singularities the grid is nonorthogonal. The combined use of vector-invariant equations and the finite-volume method is shown to avoid degeneracy at these singular points. The model is tested using experiments proposed by Williamson et al. and Held and Saurez. The atmospheric solutions are examined seeking evidence of the underlying grid in solutions and eddy statistics. A global ocean simulation is also conducted using the same code. The solutions prove to be accurate and free of artifacts arising from the... Abstract A hydrodynamical kernel that drives both an atmospheric and oceanic general circulation model is implemented in general orthogonal curvilinear coordinates using the finite-volume method on the sphere. The finite-volume method naturally describes arbitrary grids, and use of the vector-invariant form of the momentum equations simplifies the generalization to arbitrary coordinates. Grids based on the expanded spherical cube of Rancic et al., which contain eight singular points, are used. At these singularities the grid is nonorthogonal. The combined use of vector-invariant equations and the finite-volume method is shown to avoid degeneracy at these singular points. The model is tested using experiments proposed by Williamson et al. and Held and Saurez. The atmospheric solutions are examined seeking evidence of the underlying grid in solutions and eddy statistics. A global ocean simulation is also conducted using the same code. The solutions prove to be accurate and free of artifacts arising from the...Keywords
This publication has 17 references indexed in Scilit:
- An assessment of the Geophysical Fluid Dynamics Laboratory ocean model with coarse resolution: Annual‐mean climatologyJournal of Geophysical Research: Oceans, 1999
- The Use of TVD Limiters for Forward-in-Time Upstream-Biased Advection Schemes in Ocean ModelingMonthly Weather Review, 1998
- Smooth quasi‐homogeneous gridding of the sphereQuarterly Journal of the Royal Meteorological Society, 1998
- Representation of Topography by Shaved Cells in a Height Coordinate Ocean ModelMonthly Weather Review, 1997
- Hydrostatic, quasi‐hydrostatic, and nonhydrostatic ocean modelingJournal of Geophysical Research: Oceans, 1997
- A finite‐volume, incompressible Navier Stokes model for studies of the ocean on parallel computersJournal of Geophysical Research: Oceans, 1997
- Semi-Lagrangian Advection on Conformal-Cubic GridsMonthly Weather Review, 1996
- A Positive Finite-Difference Advection SchemeJournal of Computational Physics, 1995
- A Proposal for the Intercomparison of the Dynamical Cores of Atmospheric General Circulation ModelsBulletin of the American Meteorological Society, 1994
- Method of lines and direct discretization: a comparison for linear advectionApplied Numerical Mathematics, 1994