/[MITgcm]/manual/s_algorithm/text/time_stepping.tex
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revision 1.32 by jmc, Tue Feb 26 21:23:56 2013 UTC revision 1.33 by jmc, Thu Apr 18 03:36:16 2013 UTC
# Line 924  at the same point in the code. Line 924  at the same point in the code.
924    
925    
926    
927  \subsection{Crank-Nickelson barotropic time stepping}  \subsection{Crank-Nicolson barotropic time stepping}
928  \label{sec:freesurf-CrankNick}  \label{sec:freesurf-CrankNick}
929    
930  The full implicit time stepping described previously is  The full implicit time stepping described previously is
# Line 936  for the barotropic flow divergence ($\ga Line 936  for the barotropic flow divergence ($\ga
936  \\  \\
937  For instance, $\beta=\gamma=1$ is the previous fully implicit scheme;  For instance, $\beta=\gamma=1$ is the previous fully implicit scheme;
938  $\beta=\gamma=1/2$ is the non damping (energy conserving), unconditionally  $\beta=\gamma=1/2$ is the non damping (energy conserving), unconditionally
939  stable, Crank-Nickelson scheme; $(\beta,\gamma)=(1,0)$ or $=(0,1)$  stable, Crank-Nicolson scheme; $(\beta,\gamma)=(1,0)$ or $=(0,1)$
940  corresponds to the forward - backward scheme that conserves energy but is  corresponds to the forward - backward scheme that conserves energy but is
941  only stable for small time steps.\\  only stable for small time steps.\\
942  In the code, $\beta,\gamma$ are defined as parameters, respectively  In the code, $\beta,\gamma$ are defined as parameters, respectively
# Line 999  to the free-surface variations ($\epsilo Line 999  to the free-surface variations ($\epsilo
999  {\bf useRealFreshWater}{\em=TRUE} in parameter file {\em data}).  {\bf useRealFreshWater}{\em=TRUE} in parameter file {\em data}).
1000  In order to remain consistent with the tracer equation, specially in  In order to remain consistent with the tracer equation, specially in
1001  the non-linear free-surface formulation, this term is also  the non-linear free-surface formulation, this term is also
1002  affected by the Crank-Nickelson time stepping. The RHS reads:  affected by the Crank-Nicolson time stepping. The RHS reads:
1003  $\epsilon_{fw} ( \gamma (P-E)^{n+1/2} + (1-\gamma) (P-E)^{n-1/2} )$  $\epsilon_{fw} ( \gamma (P-E)^{n+1/2} + (1-\gamma) (P-E)^{n-1/2} )$
1004  %\item The non-hydrostatic part of the code has not yet been  %\item The non-hydrostatic part of the code has not yet been
1005  %updated, and therefore cannot be used with $(\beta,\gamma) \neq (1,1)$.  %updated, and therefore cannot be used with $(\beta,\gamma) \neq (1,1)$.
1006  \item The stability criteria with Crank-Nickelson time stepping  \item The stability criteria with Crank-Nicolson time stepping
1007  for the pure linear gravity wave problem in cartesian coordinates is:  for the pure linear gravity wave problem in cartesian coordinates is:
1008  \begin{itemize}  \begin{itemize}
1009  \item $\beta + \gamma < 1$ : unstable  \item $\beta + \gamma < 1$ : unstable

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