Changes between Version 421 and Version 422 of doc/app/initialization_parameters


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Timestamp:
Jul 9, 2019 5:35:44 PM (6 years ago)
Author:
suehring
Comment:

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  • doc/app/initialization_parameters

    v421 v422  
    12161216'''Note''': Due to the larger stencil of this scheme vertical grid stretching should be handled with care.
    12171217The computation of turbulent fluxes takes place inside the advection routines to get a statistical evaluation consistent to the numerical solution. \\\\
     1218
     1219'''Note''', in case of large gradients close to poorly-resolved cavities, e.g. narrow street canyons, numerical oscillation can occur which might built-up if the flow is almost completely blocked. In this case it is recommended to apply a monotonic flux limiter ([#monotonic_limiter_z monotonic_limiter_z] = .T.) which guarantees monotone and positive definite vertical advection of passive scalars (only). 
     1220
    12181221'' 'pw-scheme' ''\\\\
    12191222      The scheme of Piacsek and Williams (1970, J. Comp. Phys., 6, 392-405) with central differences in the form C3 is used.\\\\