Changeset 10419 for NEMO/branches/2018/dev_r10164_HPC09_ESIWACE_PREP_MERGE/doc/latex/NEMO/subfiles/chap_CONFIG.tex
- Timestamp:
- 2018-12-19T20:46:30+01:00 (5 years ago)
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- NEMO/branches/2018/dev_r10164_HPC09_ESIWACE_PREP_MERGE/doc/latex
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NEMO/branches/2018/dev_r10164_HPC09_ESIWACE_PREP_MERGE/doc/latex/NEMO/subfiles/chap_CONFIG.tex
r10368 r10419 1 \documentclass[../tex_main/NEMO_manual]{subfiles} 1 \documentclass[../main/NEMO_manual]{subfiles} 2 2 3 \begin{document} 3 4 % ================================================================ 4 % Chapter �Configurations5 % Chapter Configurations 5 6 % ================================================================ 6 7 \chapter{Configurations} 7 8 \label{chap:CFG} 9 8 10 \minitoc 9 11 10 12 \newpage 11 $\ $\newline % force a new ligne12 13 13 14 % ================================================================ … … 16 17 \section{Introduction} 17 18 \label{sec:CFG_intro} 18 19 19 20 20 The purpose of this part of the manual is to introduce the \NEMO reference configurations. … … 36 36 \label{sec:CFG_c1d} 37 37 38 $\ $\newline39 38 BE careful: to be re-written according to suppression of jpizoom and jpjzoom !!!! 40 $\ $\newline41 39 42 40 The 1D model option simulates a stand alone water column within the 3D \NEMO system. … … 102 100 \begin{center} 103 101 \includegraphics[width=0.98\textwidth]{Fig_ORCA_NH_mesh} 104 \caption{ \protect\label{fig:MISC_ORCA_msh} 102 \caption{ 103 \protect\label{fig:MISC_ORCA_msh} 105 104 ORCA mesh conception. 106 105 The departure from an isotropic Mercator grid start poleward of 20\degN. … … 108 107 are determined analytically and form the i-lines of the ORCA mesh (pseudo latitudes). 109 108 Then, following \citet{Madec_Imbard_CD96}, the normal to the series of ellipses (red curves) is computed which 110 provides the j-lines of the mesh (pseudo longitudes). } 109 provides the j-lines of the mesh (pseudo longitudes). 110 } 111 111 \end{center} 112 112 \end{figure} … … 133 133 \includegraphics[width=1.0\textwidth]{Fig_ORCA_NH_msh05_e1_e2} 134 134 \includegraphics[width=0.80\textwidth]{Fig_ORCA_aniso} 135 \caption { \protect\label{fig:MISC_ORCA_e1e2} 135 \caption { 136 \protect\label{fig:MISC_ORCA_e1e2} 136 137 \textit{Top}: Horizontal scale factors ($e_1$, $e_2$) and 137 138 \textit{Bottom}: ratio of anisotropy ($e_1 / e_2$) … … 139 140 South of 20\degN a Mercator grid is used ($e_1 = e_2$) so that the anisotropy ratio is 1. 140 141 Poleward of 20\degN, the two "north pole" introduce a weak anisotropy over the ocean areas ($< 1.2$) except in 141 vicinity of Victoria Island (Canadian Arctic Archipelago). } 142 \end{center} \end{figure} 143 %>>>>>>>>>>>>>>>>>>>>>>>>>>>> 144 142 vicinity of Victoria Island (Canadian Arctic Archipelago). 143 } 144 \end{center} 145 \end{figure} 146 %>>>>>>>>>>>>>>>>>>>>>>>>>>>> 145 147 146 148 The method is applied to Mercator grid ($i.e.$ same zonal and meridional grid spacing) poleward of 20\degN, … … 161 163 \label{subsec:CFG_orca_resolution} 162 164 163 164 165 The NEMO system is provided with five built-in ORCA configurations which differ in the horizontal resolution. 165 166 The value of the resolution is given by the resolution at the Equator expressed in degrees. … … 169 170 (Tab. \autoref{tab:ORCA}). 170 171 171 172 173 174 172 %--------------------------------------------------TABLE-------------------------------------------------- 175 \begin{table}[!t] \begin{center} 176 \begin{tabular}{p{4cm} c c c c} 177 Horizontal Grid & \np{ORCA\_index} & \np{jpiglo} & \np{jpjglo} & \\ 178 \hline \hline 179 \~4\deg & 4 & 92 & 76 & \\ 180 \~2\deg & 2 & 182 & 149 & \\ 181 \~1\deg & 1 & 362 & 292 & \\ 182 \~0.5\deg & 05 & 722 & 511 & \\ 183 \~0.25\deg & 025 & 1442 & 1021 & \\ 184 %\key{orca\_r8} & 8 & 2882 & 2042 & \\ 185 %\key{orca\_r12} & 12 & 4322 & 3062 & \\ 186 \hline \hline 187 \end{tabular} 188 \caption{ \protect\label{tab:ORCA} 189 Domain size of ORCA family configurations. 190 The flag for configurations of ORCA family need to be set in \textit{domain\_cfg} file. } 191 \end{center} 173 \begin{table}[!t] 174 \begin{center} 175 \begin{tabular}{p{4cm} c c c c} 176 Horizontal Grid & \np{ORCA\_index} & \np{jpiglo} & \np{jpjglo} & \\ 177 \hline 178 \hline 179 \~4\deg & 4 & 92 & 76 & \\ 180 \~2\deg & 2 & 182 & 149 & \\ 181 \~1\deg & 1 & 362 & 292 & \\ 182 \~0.5\deg & 05 & 722 & 511 & \\ 183 \~0.25\deg & 025 & 1442 & 1021 & \\ 184 % \key{orca\_r8} & 8 & 2882 & 2042 & \\ 185 % \key{orca\_r12} & 12 & 4322 & 3062 & \\ 186 \hline 187 \hline 188 \end{tabular} 189 \caption{ 190 \protect\label{tab:ORCA} 191 Domain size of ORCA family configurations. 192 The flag for configurations of ORCA family need to be set in \textit{domain\_cfg} file. 193 } 194 \end{center} 192 195 \end{table} 193 196 %-------------------------------------------------------------------------------------------------------------- … … 284 287 \begin{center} 285 288 \includegraphics[width=1.0\textwidth]{Fig_GYRE} 286 \caption{ \protect\label{fig:GYRE} 289 \caption{ 290 \protect\label{fig:GYRE} 287 291 Snapshot of relative vorticity at the surface of the model domain in GYRE R9, R27 and R54. 288 From \citet{Levy_al_OM10}.} 292 From \citet{Levy_al_OM10}. 293 } 289 294 \end{center} 290 295 \end{figure} … … 315 320 Unlike ordinary river points the Baltic inputs also include salinity and temperature data. 316 321 322 \biblio 323 317 324 \end{document}
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