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Revision 1.2 - (hide annotations) (download) (as text)
Wed Jun 4 13:29:45 2008 UTC (17 years, 1 month ago) by mlosch
Branch: MAIN
CVS Tags: end_of_ceaice_monolith, HEAD
Changes since 1.1: +24 -13 lines
File MIME type: application/x-tex
remove place holder and put in a list of (tentative) recommendations
that we may want to give

1 dimitri 1.1 \section{Discussion and conclusion}
2     \label{sec:concl}
3    
4 mlosch 1.2 Recommendations
5     \begin{itemize}
6     \item use the LSOR or another implicit solver, because EVP tends to
7     have too weak ice, and is much slower for the recommended time step
8     choices ($\frac{1}{120}$ of the model time step). Linearization does
9     not appear to be an issue for the short time steps used in this
10     study ($\Delta{t} = 20\text{\,min}$), and the LSOR-solver converges
11     quickly (only a few iterations) at each time step, because the
12     forcing changes only slowly within 20\,min.
13     \item thermodynamics appears to thave the second largest effect (after
14     EVP vs.\ LSOR)
15     \item use a flux limited scheme without explicit diffusion for
16     advecting thermodynamic variables
17     \item use no slip boundary conditions, they make more sense
18     \item TEM has little effect on the solution, other rheologies that
19     differ more from the elliptic yield curve may have bigger effects
20     \item the effects of \citet{hibler87}'s stress formulation on both ice
21     and ocean model need further exploration
22     \end{itemize}
23    
24     %%% Local Variables:
25     %%% mode: latex
26     %%% TeX-master: "ceaice"
27     %%% End:

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