Changeset 2981
- Timestamp:
- 2011-10-24T14:48:33+02:00 (13 years ago)
- Location:
- branches/2011/dev_r2802_UKMO8_cice/DOC/TexFiles/Chapters
- Files:
-
- 2 edited
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branches/2011/dev_r2802_UKMO8_cice/DOC/TexFiles/Chapters/Chap_SBC.tex
r2541 r2981 909 909 ice-ocean fluxes, that are combined with the air-sea fluxes using the ice fraction of 910 910 each model cell to provide the surface ocean fluxes. Note that the activation of a 911 sea-ice model is is done by defining a CPP key (\key{lim2} or \key{lim3}).912 The activation automatically ove writethe read value of nn{\_}ice to its appropriate913 value ($i.e.$ $2$ for LIM-2 and $3$ for LIM-3).911 sea-ice model is is done by defining a CPP key (\key{lim2}, \key{lim3} or \key{cice}). 912 The activation automatically overwrites the read value of nn{\_}ice to its appropriate 913 value ($i.e.$ $2$ for LIM-2, $3$ for LIM-3 or $4$ for CICE). 914 914 \end{description} 915 915 916 916 % {Description of Ice-ocean interface to be added here or in LIM 2 and 3 doc ?} 917 918 \subsection [Interface to CICE (\textit{sbcice\_cice})] 919 {Interface to CICE (\mdl{sbcice\_cice})} 920 \label{SBC_cice} 921 922 It is now possible to couple a global NEMO configuration (without AGRIF) to the CICE sea-ice 923 model by using \key{cice}. The CICE code can be obtained from 924 \href{http://oceans11.lanl.gov/trac/CICE/}{LANL} and the additional 'hadgem3' drivers will be required, 925 even with the latest code release. Input grid files consistent with those used in NEMO will also be needed, 926 and CICE CPP keys \bf{ORCA_GRID}, \bf{CICE_IN_NEMO} and \bf{coupled} should be used (seek advice from UKMO 927 if necessary). Currently the code is only designed to work when using the CORE forcing option for NEMO (with 928 \textit{calc\_strair~=~true} and \textit{calc\_Tsfc~=~true} in the CICE name-list), or alternatively when NEMO 929 is coupled to the HadGAM3 atmosphere model. 930 931 There are two options for the technical coupling between NEMO and CICE. The standard version allows 932 complete flexibility for the domain decompositions in the individual models, but this is at the expense of global 933 gather and scatter operations in the coupling which become very expensive on larger numbers of processors. The 934 alternative option (using \key{nemocice_decomp} for both NEMO and CICE) ensures that the domain decomposition is 935 identical in both models (provided domain parameters are set appropriately, and 936 \textit{processor\_shape~=~square-ice} and \textit{distribution\_wght~=~block} in the CICE name-list) and allows 937 much more efficient direct coupling on individual processors. This solution scales much better although it is at 938 the expense of having more idle CICE processors in areas where there is no sea ice. 939 917 940 918 941 % ------------------------------------------------------------------------------------------------------------- -
branches/2011/dev_r2802_UKMO8_cice/DOC/TexFiles/Chapters/Introduction.tex
r2570 r2981 63 63 \citep{OASIS2006}. Two-way nesting is also available through an interface to the 64 64 AGRIF package (Adaptative Grid Refinement in \textsc{Fortran}) \citep{Debreu_al_CG2008}. 65 The interface code for coupling to an alternative sea ice model (CICE, \citet{Hunke2008}) is now 66 available although this is currently only designed for global domains, without the use of AGRIF. 65 67 66 68 Other model characteristics are the lateral boundary conditions (chapter~\ref{LBC}).
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