[10567] | 1 | \documentclass{article} |
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| 2 | |
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| 3 | \usepackage{xspace, natbib, minted} |
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| 4 | |
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| 5 | \setminted{style=emacs, fontsize=\scriptsize, breaklines, frame=leftline} |
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| 6 | |
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| 7 | \renewcommand{\deg}{$^{\circ} $ \xspace} |
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| 8 | \newcommand{\ifile}[1]{\textit{#1.nc}\index{Input NetCDF files!#1.nc}} |
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| 9 | \newcommand{\mdl}[1]{\textit{#1.F90}\index{Modules!#1}} |
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| 10 | \newcommand{\ngn}[1]{\textit{#1}\index{Namelist Group Name!#1}} |
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| 11 | \newcommand{\np}[1]{\textit{#1}\index{Namelist variables!#1}} |
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| 12 | |
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| 13 | \begin{document} |
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| 14 | |
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| 15 | DMP\_TOOLS can be used to generate a netcdf file containing the restoration coefficient $\gamma$. |
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| 16 | Note that in order to maintain bit comparison with previous NEMO versions DMP\_TOOLS must be compiled and |
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| 17 | run on the same machine as the NEMO model. |
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| 18 | A \ifile{mesh\_mask} file for the model configuration is required as an input. |
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| 19 | This can be generated by carrying out a short model run with the namelist parameter \np{nn\_msh} set to 1. |
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| 20 | The namelist parameter \np{ln\_tradmp} will also need to be set to .false. for this to work. |
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| 21 | The \ngn{nam\_dmp\_create} namelist in the DMP\_TOOLS directory is used to specify options for |
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| 22 | the restoration coefficient. |
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| 23 | |
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| 24 | %--------------------------------------------nam_dmp_create------------------------------------------------- |
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| 25 | \inputminted{fortran}{./namelist} |
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| 26 | %------------------------------------------------------------------------------------------------------- |
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| 27 | |
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| 28 | \np{cp\_cfg}, \np{cp\_cpz}, \np{jp\_cfg} and \np{jperio} specify the model configuration being used and |
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| 29 | should be the same as specified in \ngn{namcfg}. |
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| 30 | The variable \np{lzoom} is used to specify that the damping is being used as in case \textit{a} above to |
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| 31 | provide boundary conditions to a zoom configuration. |
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| 32 | In the case of the arctic or antarctic zoom configurations this includes some specific treatment. |
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| 33 | Otherwise damping is applied to the 6 grid points along the ocean boundaries. |
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| 34 | The open boundaries are specified by the variables \np{lzoom\_n}, \np{lzoom\_e}, \np{lzoom\_s}, \np{lzoom\_w} in |
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| 35 | the \ngn{nam\_zoom\_dmp} namelist. |
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| 36 | |
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| 37 | The remaining switch namelist variables determine the spatial variation of the restoration coefficient in |
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| 38 | non-zoom configurations. |
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| 39 | \np{ln\_full\_field} specifies that newtonian damping should be applied to the whole model domain. |
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| 40 | \np{ln\_med\_red\_seas} specifies grid specific restoration coefficients in the Mediterranean Sea for |
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| 41 | the ORCA4, ORCA2 and ORCA05 configurations. |
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| 42 | If \np{ln\_old\_31\_lev\_code} is set then the depth variation of the coeffients will be specified as |
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| 43 | a function of the model number. |
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| 44 | This option is included to allow backwards compatability of the ORCA2 reference configurations with |
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| 45 | previous model versions. |
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| 46 | \np{ln\_coast} specifies that the restoration coefficient should be reduced near to coastlines. |
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| 47 | This option only has an effect if \np{ln\_full\_field} is true. |
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| 48 | \np{ln\_zero\_top\_layer} specifies that the restoration coefficient should be zero in the surface layer. |
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| 49 | Finally \np{ln\_custom} specifies that the custom module will be called. |
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| 50 | This module is contained in the file \mdl{custom} and can be edited by users. |
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| 51 | For example damping could be applied in a specific region. |
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| 52 | |
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| 53 | The restoration coefficient can be set to zero in equatorial regions by |
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| 54 | specifying a positive value of \np{nn\_hdmp}. |
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| 55 | Equatorward of this latitude the restoration coefficient will be zero with a smooth transition to |
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| 56 | the full values of a 10\deg latitud band. |
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| 57 | This is often used because of the short adjustment time scale in the equatorial region |
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| 58 | \citep{Reverdin1991, Fujio1991, Marti_PhD92}. |
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| 59 | The time scale associated with the damping depends on the depth as a hyperbolic tangent, |
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| 60 | with \np{rn\_surf} as surface value, \np{rn\_bot} as bottom value and a transition depth of \np{rn\_dep}. |
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| 61 | |
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| 62 | \bibliography{doc_DMP_tool} |
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| 63 | \bibliographystyle{plainnat} |
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| 64 | |
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| 65 | \end{document} |
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