Index: NEMO/branches/2020/dev_r14116_HPC-04_mcastril_Mixed_Precision_implementation_final/doc/latex/NEMO/subfiles/chap_DOM.tex
===================================================================
--- NEMO/branches/2020/dev_r14116_HPC-04_mcastril_Mixed_Precision_implementation_final/doc/latex/NEMO/subfiles/chap_DOM.tex	(revision 14197)
+++ NEMO/branches/2020/dev_r14116_HPC-04_mcastril_Mixed_Precision_implementation_final/doc/latex/NEMO/subfiles/chap_DOM.tex	(revision 14644)
@@ -14,6 +14,4 @@
 % -    domclo: closed sea and lakes....
 %              management of closea sea area: specific to global cfg, both forced and coupled
-
-\thispagestyle{plain}
 
 \chaptertoc
@@ -368,6 +366,6 @@
 \label{subsec:DOM_size}
 
-The total size of the computational domain is set by the parameters \jp{jpiglo}, \jp{jpjglo} and
-\jp{jpkglo} for the $i$, $j$ and $k$ directions, respectively.
+The total size of the computational domain is set by the parameters \texttt{jpiglo}, \texttt{jpjglo} and
+\texttt{jpkglo} for the $i$, $j$ and $k$ directions, respectively.
 Note, that the variables \texttt{jpi} and \texttt{jpj} refer to
 the size of each processor subdomain when the code is run in parallel using domain decomposition
@@ -379,7 +377,7 @@
 in which case \np{cn_cfg}{cn\_cfg} and \np{nn_cfg}{nn\_cfg} are set from these values accordingly).
 
-The global lateral boundary condition type is selected from 8 options using parameter \jp{jperio}.
+The global lateral boundary condition type is selected from 8 options using parameters \texttt{l\_Iperio}, \texttt{l\_Jperio}, \texttt{l\_NFold} and \texttt{c\_NFtype}.
 See \autoref{sec:LBC_jperio} for details on the available options and
-the corresponding values for \jp{jperio}.
+the corresponding values for \texttt{l\_Iperio}, \texttt{l\_Jperio}, \texttt{l\_NFold} and \texttt{c\_NFtype}.
 
 %% =================================================================================================
@@ -396,10 +394,12 @@
 
 \begin{clines}
-int    jpiglo, jpjglo, jpkglo     /* global domain sizes                                    */
-int    jperio                     /* lateral global domain b.c.                             */
-double glamt, glamu, glamv, glamf /* geographic longitude (t,u,v and f points respectively) */
-double gphit, gphiu, gphiv, gphif /* geographic latitude                                    */
-double e1t, e1u, e1v, e1f         /* horizontal scale factors                               */
-double e2t, e2u, e2v, e2f         /* horizontal scale factors                               */
+integer   Ni0glo, NjOglo, jpkglo       /* global domain sizes (without MPI halos)                */
+logical   l\_Iperio, l\_Jperio         /* lateral global domain b.c.: i- j-periodicity           */
+logical   l\_NFold                     /* lateral global domain b.c.: North Pole folding         */
+char(1)   c\_NFtype                    /*    type of North pole Folding: T or F point            */
+real      glamt, glamu, glamv, glamf   /* geographic longitude (t,u,v and f points respectively) */
+real      gphit, gphiu, gphiv, gphif   /* geographic latitude                                    */
+real      e1t, e1u, e1v, e1f           /* horizontal scale factors                               */
+real      e2t, e2u, e2v, e2f           /* horizontal scale factors                               */
 \end{clines}
 
@@ -465,5 +465,5 @@
 \begin{enumerate}
 \item the bathymetry given in meters;
-\item the number of levels of the model (\jp{jpk});
+\item the number of levels of the model (\texttt{jpk});
 \item the analytical transformation $z(i,j,k)$ and the vertical scale factors
   (derivatives of the transformation); and
@@ -575,6 +575,6 @@
 every gridcell in the model regardless of the choice of vertical coordinate.
 With constant z-levels, e3 metrics will be uniform across each horizontal level.
-In the partial step case each e3 at the \jp{bottom\_level}
-(and, possibly, \jp{top\_level} if ice cavities are present)
+In the partial step case each e3 at the \texttt{bottom\_level}
+(and, possibly, \texttt{top\_level} if ice cavities are present)
 may vary from its horizontal neighbours.
 And, in s-coordinates, variations can occur throughout the water column.
@@ -585,8 +585,8 @@
 those arising from a flat sea surface with zero elevation.
 
-The \jp{bottom\_level} and \jp{top\_level} 2D arrays define
-the \jp{bottom\_level} and top wet levels in each grid column.
-Without ice cavities, \jp{top\_level} is essentially a land mask (0 on land; 1 everywhere else).
-With ice cavities, \jp{top\_level} determines the first wet point below the overlying ice shelf.
+The \texttt{bottom\_level} and \texttt{top\_level} 2D arrays define
+the \texttt{bottom\_level} and top wet levels in each grid column.
+Without ice cavities, \texttt{top\_level} is essentially a land mask (0 on land; 1 everywhere else).
+With ice cavities, \texttt{top\_level} determines the first wet point below the overlying ice shelf.
 
 %% =================================================================================================
@@ -594,5 +594,5 @@
 \label{subsec:DOM_msk}
 
-From \jp{top\_level} and \jp{bottom\_level} fields, the mask fields are defined as follows:
+From \texttt{top\_level} and \texttt{bottom\_level} fields, the mask fields are defined as follows:
 \begin{align*}
   tmask(i,j,k) &=
