IMEX and Semi-Implicit Runge-Kutta Schemes for CFD Simulations
Numerical Weather Prediction (NWP) and climate models parametrize the effects of boundary-layer turbulence as a diffusive process, dependent on a diffusion coefficient, which appears as nonlinear terms in the governing equations. In the advection dominated zone of the boundary layer and in the free...
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| Format: | Others |
| Language: | en |
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Université d'Ottawa / University of Ottawa
2018
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| Online Access: | http://hdl.handle.net/10393/37957 http://dx.doi.org/10.20381/ruor-22215 |