A horror story about integration methods
Journal of Computational Physics
MPDATA: a finite-difference solver for geophysical flows
Journal of Computational Physics
Composite Schemes for Conservation Laws
SIAM Journal on Numerical Analysis
Large-eddy simulations of convective boundary layers using nonoscillatory differencing
Physica D - Special issue originating from the 18th Annual International Conference of the Center for Nonlinear Studies, Los Alamos, NM, May 11&mdash ;15, 1998
Pattern Recognition and Neural Networks
Pattern Recognition and Neural Networks
An all-scale anelastic model for geophysical flows: dynamic grid deformation
Journal of Computational Physics
Journal of Computational Physics
An adaptive local deconvolution method for implicit LES
Journal of Computational Physics
Building resolving large-eddy simulations and comparison with wind tunnel experiments
Journal of Computational Physics
Nonhydrostatic icosahedral atmospheric model (NICAM) for global cloud resolving simulations
Journal of Computational Physics
A time-split nonhydrostatic atmospheric model for weather research and forecasting applications
Journal of Computational Physics
Iterated upwind schemes for gas dynamics
Journal of Computational Physics
PPAM'09 Proceedings of the 8th international conference on Parallel processing and applied mathematics: Part II
EULAG, a computational model for multiscale flows: An MHD extension
Journal of Computational Physics
An unstructured-mesh atmospheric model for nonhydrostatic dynamics
Journal of Computational Physics
Hi-index | 31.46 |
Astounded at the regularity of convective structures observed in simulations of mesoscale flow past realistic topography, we investigate the computational aspects of a classical problem of flow over a heated plane. We find that the numerical solutions are sensitive to viscosity, either incorporated a priori or effectively realized in computational models. In particular, anisotropic viscosity can lead to regular convective structures that mimic naturally realizable Rayleigh-Benard cells, which are unphysical for the specified external parameter range. Details of the viscosity appear to play a secondary role; that is, similar structures can occur for prescribed constant viscosities, explicit subgrid-scale turbulence models, ad-hoc numerical filters, or implicit dissipation of numerical schemes. This implies the need for a careful selection of numerical tools suitable for convection-resolving simulations of atmospheric circulations. The implicit large-eddy-simulation (ILES) approach using non-oscillatory schemes is especially attractive, as for under-resolved calculations it reproduces well the coarsened results of finely-resolved boundary layer convection.