Changeset 9407 for branches/2017/dev_merge_2017/DOC/tex_sub/chap_misc.tex
- Timestamp:
- 2018-03-15T17:40:35+01:00 (6 years ago)
- File:
-
- 1 edited
Legend:
- Unmodified
- Added
- Removed
-
branches/2017/dev_merge_2017/DOC/tex_sub/chap_misc.tex
r9394 r9407 5 5 % ================================================================ 6 6 \chapter{Miscellaneous Topics} 7 \label{ MISC}7 \label{chap:MISC} 8 8 \minitoc 9 9 … … 15 15 % ================================================================ 16 16 \section{Representation of unresolved straits} 17 \label{ MISC_strait}17 \label{sec:MISC_strait} 18 18 19 19 In climate modeling, it often occurs that a crucial connections between water masses … … 43 43 % ------------------------------------------------------------------------------------------------------------- 44 44 \subsection{Hand made geometry changes} 45 \label{ MISC_strait_hand}45 \label{subsec:MISC_strait_hand} 46 46 47 47 $\bullet$ reduced scale factor in the cross-strait direction to a value in better agreement 48 with the true mean width of the strait. ( Fig.~\ref{Fig_MISC_strait_hand}).48 with the true mean width of the strait. (\autoref{fig:MISC_strait_hand}). 49 49 This technique is sometime called "partially open face" or "partially closed cells". 50 50 The key issue here is only to reduce the faces of $T$-cell ($i.e.$ change the value … … 56 56 57 57 $\bullet$ increase of the viscous boundary layer thickness by local increase of the 58 fmask value at the coast ( Fig.~\ref{Fig_MISC_strait_hand}). This is done in58 fmask value at the coast (\autoref{fig:MISC_strait_hand}). This is done in 59 59 \mdl{dommsk} together with the setting of the coastal value of fmask 60 (see Section \ref{LBC_coast})60 (see \autoref{sec:LBC_coast}) 61 61 62 62 %>>>>>>>>>>>>>>>>>>>>>>>>>>>> … … 64 64 \includegraphics[width=0.80\textwidth]{Fig_Gibraltar} 65 65 \includegraphics[width=0.80\textwidth]{Fig_Gibraltar2} 66 \caption{ \protect\label{ Fig_MISC_strait_hand}66 \caption{ \protect\label{fig:MISC_strait_hand} 67 67 Example of the Gibraltar strait defined in a $1^{\circ} \times 1^{\circ}$ mesh. 68 68 \textit{Top}: using partially open cells. The meridional scale factor at $v$-point … … 71 71 \textit{Bottom}: using viscous boundary layers. The four fmask parameters 72 72 along the strait coastlines are set to a value larger than 4, $i.e.$ "strong" no-slip 73 case (see Fig.\ref{Fig_LBC_shlat}) creating a large viscous boundary layer73 case (see \autoref{fig:LBC_shlat}) creating a large viscous boundary layer 74 74 that allows a reduced transport through the strait.} 75 75 \end{center} \end{figure} … … 81 81 % ================================================================ 82 82 \section{Closed seas (\protect\mdl{closea})} 83 \label{ MISC_closea}83 \label{sec:MISC_closea} 84 84 85 85 \colorbox{yellow}{Add here a short description of the way closed seas are managed} … … 90 90 % ================================================================ 91 91 \section{Sub-domain functionality} 92 \label{ MISC_zoom}92 \label{sec:MISC_zoom} 93 93 94 94 \subsection{Simple subsetting of input files via NetCDF attributes} … … 140 140 \begin{figure}[!ht] \begin{center} 141 141 \includegraphics[width=0.90\textwidth]{Fig_LBC_zoom} 142 \caption{ \protect\label{ Fig_LBC_zoom}142 \caption{ \protect\label{fig:LBC_zoom} 143 143 Position of a model domain compared to the data input domain when the zoom functionality is used.} 144 144 \end{center} \end{figure} … … 150 150 % ================================================================ 151 151 \section{Accuracy and reproducibility (\protect\mdl{lib\_fortran})} 152 \label{ MISC_fortran}152 \label{sec:MISC_fortran} 153 153 154 154 \subsection{Issues with intrinsinc SIGN function (\protect\key{nosignedzero})} 155 \label{ MISC_sign}155 \label{subsec:MISC_sign} 156 156 157 157 The SIGN(A, B) is the \textsc {Fortran} intrinsic function delivers the magnitude … … 179 179 180 180 \subsection{MPP reproducibility} 181 \label{ MISC_glosum}181 \label{subsec:MISC_glosum} 182 182 183 183 The numerical reproducibility of simulations on distributed memory parallel computers … … 207 207 208 208 \subsection{MPP scalability} 209 \label{ MISC_mppsca}209 \label{subsec:MISC_mppsca} 210 210 211 211 The default method of communicating values across the north-fold in distributed memory applications … … 231 231 % ================================================================ 232 232 \section{Model optimisation, control print and benchmark} 233 \label{ MISC_opt}233 \label{sec:MISC_opt} 234 234 %--------------------------------------------namctl------------------------------------------------------- 235 235 \forfile{../namelists/namctl} … … 270 270 271 271 $\bullet$ Benchmark (\np{nn\_bench}). This option defines a benchmark run based on 272 a GYRE configuration (see \ S\ref{CFG_gyre}) in which the resolution remains the same272 a GYRE configuration (see \autoref{sec:CFG_gyre}) in which the resolution remains the same 273 273 whatever the domain size. This allows a very large model domain to be used, just by 274 274 changing the domain size (\jp{jpiglo}, \jp{jpjglo}) and without adjusting either the time-step
Note: See TracChangeset
for help on using the changeset viewer.
