Changes between Version 4 and Version 5 of doc/tec/discret


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Timestamp:
Apr 14, 2016 1:02:10 PM (8 years ago)
Author:
Giersch
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  • doc/tec/discret

    v4 v5  
    1212
    1313It is thus possible to calculate the derivatives of the velocity components at the center of the volumes (same location as the scalars). By the same token, derivatives of scalar quantities can be calculated at the edges of the volumes. In this way it is possible to calculate derivatives over only one grid length and the effective spatial model resolution can be increased by a factor of two in comparison to non-staggered grids.
     14By default, the advection terms in the first five equations in Sect. [wiki:doc/tec/gov governing equations] are discretized using an upwind-biased 5th-order differencing scheme in combination with a 3rd-order Runge–Kutta  time-stepping scheme after [#williamson Williamson (1980)]. [#wicker Wicker and Skamarock(2002)] compared different time- and advection differencing schemes and found that this combination give the best results regarding accuracy and algorithmic simplicity. However, the 5th-order differencing scheme is known to be overly dissipative. It is thus also possible to use a 2nd-order scheme after \citet{piacsek1970}. The latter scheme is non-dissipative, but it suffers from immense numerical dispersion. Time discretization can also be achieved using 2nd-order Runge–Kutta or 1st-order Euler schemes.
    1415
     16\bibitem[{Wicker and Skamarock(2002)}]{wicker2002} Wicker,~L.~J. and
     17  Skamarock,~W.~C.: {Time-splitting methods for elastic models using
     18    forward time schemes}, Mon. Weather Rev., 130, 2088--2097,
     19  2002.
    1520
    1621== References ==
     
    1924* [=#arakawa]'''Schumann U.''' 1977. Computational design of the basic dynamical processes of the UCLA general circulation model. in: General
    2025  Circulation Models of the Atmosphere, Methods in Computational Physics. edited by: Chang J. 17. Berlin. 173–265.
     26
     27* [=#williamson]'''Williamson JH.''' 1980. Low-storage Runge–Kutta schemes. J. Comput. Phys. 35: 48–56.
     28
     29* [=#wicker]'''Wicker LJ, Skamarock WC.''' 1980. Time-splitting methods for elastic models using forward time schemes. Mon. Weather Rev. 130: 2088–2097.