New URL for NEMO forge!   http://forge.nemo-ocean.eu

Since March 2022 along with NEMO 4.2 release, the code development moved to a self-hosted GitLab.
This present forge is now archived and remained online for history.
Changeset 8810 for branches/2017/dev_r7881_ENHANCE09_RK3/DOC/TexFiles – NEMO

Ignore:
Timestamp:
2017-11-24T17:14:03+01:00 (7 years ago)
Author:
flavoni
Message:

ROBUST-11_Simona-DocUserdef?: update DOC and Namelists, for usrdef routines and domain_cfg

Location:
branches/2017/dev_r7881_ENHANCE09_RK3/DOC/TexFiles/Chapters
Files:
5 edited

Legend:

Unmodified
Added
Removed

  • branches/2017/dev_r7881_ENHANCE09_RK3/DOC/TexFiles/Chapters/Chap_CFG.tex

    r7705 r8810  
    3737\section{Water column model: 1D model (C1D) (\key{c1d}) } 
    3838\label{CFG_c1d} 
     39 
     40$\ $\newline 
     41BE careful: to be re-written according to suppression of jpizoom and jpjzoom !!!! 
     42$\ $\newline 
    3943 
    4044The 1D model option simulates a stand alone water column within the 3D \NEMO system.  
    … …  
    140144than the smallest one in the southern hemisphere. 
    141145The resulting mesh is shown in Fig.~\ref{Fig_MISC_ORCA_msh} and \ref{Fig_MISC_ORCA_e1e2}  
    142 for a half a degree grid (ORCA\_R05). The smallest ocean scale factor is found in along   
    143 Antarctica, while the ratio of anisotropy remains close to one except near the Victoria Island  
     146for a half a degree grid (ORCA\_R05). 
     147The smallest ocean scale factor is found in along  Antarctica, while the ratio of anisotropy remains close to one except near the Victoria Island  
    144148in the Canadian Archipelago.  
    145149 

  • branches/2017/dev_r7881_ENHANCE09_RK3/DOC/TexFiles/Chapters/Chap_DOM.tex

    r7705 r8810  
    737737\begin{table}     \begin{center} \begin{tabular}{c||r|r|r|r} 
    738738\hline 
    739 \textbf{LEVEL}& \textbf{gdept}& \textbf{gdepw}& \textbf{e3t }& \textbf{e3w  } \\ \hline 
     739\textbf{LEVEL}& \textbf{gdept\_1d}& \textbf{gdepw\_1d}& \textbf{e3t\_1d }& \textbf{e3w\_1d  } \\ \hline 
    7407401  &  \textbf{  5.00}   &       0.00 & \textbf{ 10.00} &  10.00 \\   \hline 
    7417412  &  \textbf{15.00} &    10.00 &   \textbf{ 10.00} &  10.00 \\   \hline 

  • branches/2017/dev_r7881_ENHANCE09_RK3/DOC/TexFiles/Chapters/Chap_MISC.tex

    r7646 r8810  
    22\begin{document} 
    33% ================================================================ 
    4 % Chapter ——— Miscellaneous Topics 
     4% Chapter ---€” Miscellaneous Topics 
    55% ================================================================ 
    66\chapter{Miscellaneous Topics} 
    … …  
    8787 
    8888% ================================================================ 
    89 % Sub-Domain Functionality (\textit{nizoom, njzoom}, namelist parameters) 
    90 % ================================================================ 
    91 \section{Sub-Domain Functionality (\np{jpizoom}, \np{jpjzoom})} 
     89% Sub-Domain Functionality  
     90% ================================================================ 
     91\section{Sub-Domain Functionality} 
    9292\label{MISC_zoom} 
    93  
    94 The sub-domain functionality, also improperly called the zoom option  
    95 (improperly because it is not associated with a change in model resolution)  
    96 is a quite simple function that allows a simulation over a sub-domain of an  
    97 already defined configuration ($i.e.$ without defining a new mesh, initial  
    98 state and forcings). This option can be useful for testing the user settings  
    99 of surface boundary conditions, or the initial ocean state of a huge ocean  
    100 model configuration while having a small computer memory requirement.  
    101 It can also be used to easily test specific physics in a sub-domain (for example,  
    102 see \citep{Madec_al_JPO96} for a test of the coupling used in the global ocean  
    103 version of OPA between sea-ice and ocean model over the Arctic or Antarctic  
    104 ocean, using a sub-domain). In the standard model, this option does not  
    105 include any specific treatment for the ocean boundaries of the sub-domain:  
    106 they are considered as artificial vertical walls. Nevertheless, it is quite easy  
    107 to add a restoring term toward a climatology in the vicinity of such boundaries  
    108 (see \S\ref{TRA_dmp}). 
    109  
    110 In order to easily define a sub-domain over which the computation can be  
    111 performed, the dimension of all input arrays (ocean mesh, bathymetry,  
    112 forcing, initial state, ...) are defined as \np{jpidta}, \np{jpjdta} and \np{jpkdta}  
    113 ( in \ngn{namcfg} namelist), while the computational domain is defined through  
    114 \np{jpiglo}, \np{jpjglo} and \jp{jpk} (\ngn{namcfg} namelist). When running the  
    115 model over the whole domain, the user sets \np{jpiglo}=\np{jpidta} \np{jpjglo}=\np{jpjdta}  
    116 and \jp{jpk}=\jp{jpkdta}. When running the model over a sub-domain, the user  
    117 has to provide the size of the sub-domain, (\np{jpiglo}, \np{jpjglo}, \np{jpkglo}),  
    118 and the indices of the south western corner as \np{jpizoom} and \np{jpjzoom} in  
    119 the  \ngn{namcfg} namelist (Fig.~\ref{Fig_LBC_zoom}).  
    120  
    121 Note that a third set of dimensions exist, \jp{jpi}, \jp{jpj} and \jp{jpk} which is  
    122 actually used to perform the computation. It is set by default to \jp{jpi}=\np{jpjglo}  
    123 and \jp{jpj}=\np{jpjglo}, except for massively parallel computing where the  
    124 computational domain is laid out on local processor memories following a 2D  
    125 horizontal splitting. % (see {\S}IV.2-c) ref to the section to be updated 
    12693 
    12794\subsection{Simple subsetting of input files via netCDF attributes} 
    … …  
    165132\noindent Add the logical switch to \ngn{namcfg} in the configuration namelist and set true: 
    166133%--------------------------------------------namcfg-------------------------------------------------------- 
    167 \namdisplay{namcfg_orca1} 
     134\namdisplay{namcfg} 
    168135%-------------------------------------------------------------------------------------------------------------- 
    169136 

  • branches/2017/dev_r7881_ENHANCE09_RK3/DOC/TexFiles/Chapters/Chap_SBC.tex

    r8586 r8810  
    12681268sea-ice model is is done by defining a CPP key (\key{lim3} or \key{cice}).  
    12691269The activation automatically overwrites the read value of nn{\_}ice to its appropriate  
    1270 value ($i.e.$ $2$ for LIM-2, $3$ for LIM-3 or $4$ for CICE). 
     1270value ($i.e.$ $2$ for LIM-3 or $3$ for CICE). 
    12711271\end{description} 
    12721272 

  • branches/2017/dev_r7881_ENHANCE09_RK3/DOC/TexFiles/Chapters/Introduction.tex

    r6997 r8810  
    255255$\bullet$ The main modifications from NEMO/OPA v3.4 and  v3.6 are :\\ 
    256256\begin{enumerate} 
     257 \item ... ;  
     258\end{enumerate} 
     259 
     260 
     261 \vspace{1cm} 
     262$\bullet$ The main modifications from NEMO/OPA v3.6 and  v4.0 are :\\ 
     263\begin{enumerate} 
     264\item new definition of configurations ; 
     265\item bulk formulation ; 
    257266\item ... ;  
    258267\end{enumerate} 
    259268 
    260269 
    261  \vspace{1cm} 
    262 $\bullet$ The main modifications from NEMO/OPA v3.6 and  v4.0 are :\\ 
    263 \begin{enumerate} 
    264 \item ... ;  
    265  
    266  
    267 \end{enumerate} 
    268  
    269  
    270270\end{document} 
Note: See TracChangeset for help on using the changeset viewer.