A computationally efficient Riemann solver based shallow water model on the cubed-sphere
Abstract
A cubed-sphere grid system provides much better uniform grid point distribution compared to the conventional lat-lon grid system. A finite volume method could be used to solve the flux form shallow water equations. However, due to the non-orthogonal cubed-sphere grid, extra metric terms are necessary in the momentum equations, which requires more computational steps compared to their counterpart on an orthogonal grid. In this model, the vector-invariant shallow water equations are implemented, which has fewer non-orthogonal terms. A fast Riemann solver is derived to calculate the values of the prognostic variables at control volume interfaces for the momentum equations and to compute the fluxes for the continuity equation.
- Publication:
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AGU Fall Meeting Abstracts
- Pub Date:
- December 2013
- Bibcode:
- 2013AGUFM.A33B0212C
- Keywords:
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- 3336 ATMOSPHERIC PROCESSES Numerical approximations and analyses