Changes between Version 18 and Version 19 of doc/tec/advection


Ignore:
Timestamp:
Mar 28, 2012 10:48:23 AM (13 years ago)
Author:
suehring
Comment:

--

Legend:

Unmodified
Added
Removed
Modified
  • doc/tec/advection

    v18 v19  
    6060=== Boundaries ===
    6161
    62 Due to the large stencil of WS5, additional ghost layers are necessary on each lateral boundary of each processor subdomain to avoid local data dependencies. Therefor the exchange of ghost layers is adapted to a dynamic number of ghost layers.
    63 For the bottom and top boundaries a successive degradation from WS5 to WS3 to a 2^nd^ order scheme is required to avoid unphysical fluxes which would arise from the bottom and top ghost layers. The used 2^nd^ order scheme is based on a flux discretization to ensure consistency with the WS-schemes. The PW-scheme cannot be used, because its a skew symmetric dicretization. Furthermore an additional numerical dissipation term of 2^nd^ order, based on (Shchepetkin and McWilliams, 1998) is required for the 2^nd^ order scheme to perform a numerically stable switching of advection schemes of different order.
    64 These successive degradation is also done for the lateral radiation boundary condition at the outflow and near topography (Note: Topography is currently not implemented).
     62Due to the large stencil of WS5, additional ghost layers are necessary on each lateral boundary of each processor subdomain to avoid local data dependencies. Therefore, the exchange of ghost layers is adapted to a dynamic number of ghost layers.
     63For the bottom and top boundaries, lateral non-cyclic boundaries and near topography walls a successive degradation from WS5 to WS3 to a 1^st^ order scheme is required. The used 1^st^ order scheme is based on a flux discretization to ensure consistency with the WS-schemes. The PW-scheme cannot be used, because its a skew symmetric discretization.
    6564
    6665
     
    8685  ''J. Comput. Phys.'', '''198''', 580-616.
    8786
    88 * '''Shchepetkin, A. F. und J. C. McWilliams, 1998:''' Quasi-monotone advection schemes based on explicit locally adaptive   dissipation. ''Mon. Wea. Rev.'', '''126''', 1541-1580.
    89 
    9087* '''Wicker, L. J. und W. C. Skamarock, 2002:''' Time-splitting methods for elastic models using forward time schemes.
    9188  ''Mon. Wea. Rev.'', '''130''', 2088-2097.