Changeset 11598 for NEMO/trunk/doc/latex/NEMO/subfiles/chap_DYN.tex

Timestamp:

2019-09-25T22:00:42+02:00 (5 years ago)

Author:

nicolasmartin

Message:

Add template of versioning record at the beginning of chapters

File:

• NEMO/trunk/doc/latex/NEMO/subfiles/chap_DYN.tex (modified) (15 diffs)

NEMO/trunk/doc/latex/NEMO/subfiles/chap_DYN.tex

@@ -2 +2 @@
 
 \begin{document}
+
 \chapter{Ocean Dynamics (DYN)}
 \label{chap:DYN}
 
+\thispagestyle{plain}
+
 \chaptertoc
+
+\paragraph{Changes record} ~\\
+
+{\footnotesize
+  \begin{tabularx}{\textwidth}{l||X|X}
+    Release & Author(s) & Modifications \\
+    \hline
+    {\em   4.0} & {\em ...} & {\em ...} \\
+    {\em   3.6} & {\em ...} & {\em ...} \\
+    {\em   3.4} & {\em ...} & {\em ...} \\
+    {\em <=3.4} & {\em ...} & {\em ...}
+  \end{tabularx}
+}
+
+\clearpage
 
 Using the representation described in \autoref{chap:DOM},
@@ -149 +167 @@
 (see \autoref{subsec:DOM_Num_Index_vertical}).
 
-
 %% =================================================================================================
 \section{Coriolis and advection: vector invariant form}
@@ -301 +318 @@
   \label{fig:DYN_een_triad}
 \end{figure}
-% >>>>>>>>>>>>>>>>>>>>>>>>>>>>>>>>
 
 A key point in \autoref{eq:DYN_een_e3f} is how the averaging in the \textbf{i}- and \textbf{j}- directions is made.
@@ -387 +403 @@
 a similar split-explicit time stepping should be used on vertical advection of tracer to ensure a better stability,
 an option which is only available with a TVD scheme (see \np{ln_traadv_tvd_zts}{ln\_traadv\_tvd\_zts} in \autoref{subsec:TRA_adv_tvd}).
-
 
 %% =================================================================================================
@@ -834 +849 @@
 (see their figure 12, lower left).
 
-%>   >   >   >   >   >   >   >   >   >   >   >   >   >   >   >   >   >   >   >   >   >   >   >   >   >   >   >
 \begin{figure}[!t]
   \centering
@@ -859 +873 @@
   \label{fig:DYN_spg_ts}
 \end{figure}
-%>   >   >   >   >   >   >   >   >   >   >   >   >   >   >   >   >   >   >   >   >   >   >   >   >   >   >   >
 
 In the default case (\np[=.true.]{ln_bt_fw}{ln\_bt\_fw}),
@@ -909 +922 @@
 it is still significant as shown by \citet{levier.treguier.ea_rpt07} in the case of an analytical barotropic Kelvin wave.
 
-%>>>>>===============
 \gmcomment{               %%% copy from griffies Book
 
@@ -1028 +1040 @@
 
 }            %%end gm comment (copy of griffies book)
-
-%>>>>>===============
 
 %% =================================================================================================
@@ -1251 +1261 @@
 the snow-ice mass is taken into account when computing the surface pressure gradient.
 
-
 \gmcomment{ missing : the lateral boundary condition !!!   another external forcing
  }
@@ -1307 +1316 @@
 The final sub-section covers some additional considerations that are relevant to both schemes.
 
-
 %   Iterative limiters
 %% =================================================================================================
@@ -1336 +1344 @@
 to be its depth times its velocity. This depth is considered to be zero at ``dry'' $u$-points consistent with its
 treatment in the calculation of the flux of mass across the cell face.
-
 
 \cite{warner.defne.ea_CG13} state that in their scheme the velocity masks at the cell faces for the baroclinic
@@ -1462 +1469 @@
 directional limiter does.
 
-
 %      Surface pressure gradients
 %% =================================================================================================
@@ -1481 +1487 @@
 column.  The three possible combinations are illustrated in \autoref{fig:DYN_WAD_dynhpg}.
 
-%>>>>>>>>>>>>>>>>>>>>>>>>>>>>>>>>>>>>>>>>>>>>
 \begin{figure}[!ht]
   \centering
@@ -1491 +1496 @@
   \label{fig:DYN_WAD_dynhpg}
 \end{figure}
-%>>>>>>>>>>>>>>>>>>>>>>>>>>>>>>>>>>>>>>>>>>>>
 
 The first logical, $\mathrm{ll\_tmp1}$, is set to true if and only if the water depth at
@@ -1554 +1558 @@
 See the WAD tests MY\_DOC documention for details of the WAD test cases.
 
-
-
 %% =================================================================================================
 \section[Time evolution term (\textit{dynnxt.F90})]{Time evolution term (\protect\mdl{dynnxt})}
 \label{sec:DYN_nxt}
-
 
 Options are defined through the \nam{dom}{dom} namelist variables.