Changes between Version 330 and Version 331 of doc/app/initialization_parameters
- Timestamp:
- Jun 7, 2017 12:33:31 PM (8 years ago)
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doc/app/initialization_parameters
v330 v331 927 927 '' 'pw-scheme' ''\\\\ 928 928 The scheme of Piacsek and Williams (1970, J. Comp. Phys., 6, 392-405) with central differences in the form C3 is used. 929 '' 'up-scheme' ''\\\\ 930 First-order upstream scheme. The upstream scheme is guarantees only a stable solution in combination with [#timestep_scheme timestep_scheme] = '' 'euler' ''. Note, this scheme is very diffusive, and hence, not well-suited for turbulence-resolving simulations. 929 931 }}} 930 932 |---------------- … … 1145 1147 The Bott scheme modified by Chlond (1994, Mon. Wea. Rev., 122, 111-125). This is a conservative monotonous scheme with very small numerical diffusion and therefore very good conservation of scalar flow features. The scheme, however, is computationally very expensive both because it is expensive itself and because it does (so far) not allow specific code optimizations (e.g. cache optimization). Choice of this scheme forces the Euler time step scheme to be used for the scalar quantities. For output of horizontally averaged profiles of the resolved / total heat flux, [../d3par#data_output_pr data_output_pr] = '' 'w*pt*BC' '' / '' 'wptBC' '' should be used, instead of the standard profiles ('' 'w*pt*' '' and '' 'wpt' '') because these are too inaccurate with this scheme. However, for subdomain analysis (see [#statistic_regions statistic_regions]) exactly the reverse holds: here '' 'w*pt*BC' '' and '' 'wptBC' '' show very large errors and should not be used.\\\\ 1146 1148 This scheme is not allowed for non-cyclic lateral boundary conditions (see [#bc_lr bc_lr] and [#bc_ns bc_ns]) and requires that [#loop_optimization loop_optimization] = '' 'vector' '' is set.\\\\ 1147 A differing advection scheme can be chosen for the subgrid-scale TKE using parameter [#use_upstream_for_tke use_upstream_for_tke]. 1149 '' 'up-scheme' ''\\\\ 1150 First-order upstream scheme. The upstream scheme is guarantees only a stable solution in combination with [#timestep_scheme timestep_scheme] = '' 'euler' ''. Note, this scheme is very diffusive, and hence, not well-suited for turbulence-resolving simulations. \\\\ 1151 Remark: Independent on the choice of 'scalar_advec' and [#timestep_scheme timestep_scheme], a different advection scheme can be chosen for the subgrid-scale TKE using parameter [#use_upstream_for_tke use_upstream_for_tke]. 1148 1152 }}} 1149 1153 |----------------