Changeset 14257 for NEMO/trunk/doc/latex/NEMO/subfiles/chap_DOM.tex

Timestamp:

2021-01-04T16:13:36+01:00 (3 years ago)

Author:

nicolasmartin

Message:

Overall review of LaTeX sources (not tested completely as of now):

• Reworking global files: main document.tex, add glossary.tex, cosmetic changes...
• Ignore missing namelists (namsbc_isf, namsbc_iscpl and namptr)
• Removal of references for unused indices (\hfile, \ifile and \jp)
• Update of .svnignore and svn:ignore properties accordingly
• Split of manual abstract into a common NEMO abs for all and a specific one for each engine
• Shrinking variables names used in the frontmatter

File:

• NEMO/trunk/doc/latex/NEMO/subfiles/chap_DOM.tex (modified) (7 diffs)

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

@@ -14 +14 @@
 % -    domclo: closed sea and lakes....
 %              management of closea sea area: specific to global cfg, both forced and coupled
-
-\thispagestyle{plain}
 
 \chaptertoc
@@ -368 +366 @@
 \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 +377 @@
 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 parameter \texttt{jperio}.
 See \autoref{sec:LBC_jperio} for details on the available options and
-the corresponding values for \jp{jperio}.
+the corresponding values for \texttt{jperio}.
 
 %% =================================================================================================
@@ -465 +463 @@
 \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 +573 @@
 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 +583 @@
 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 +592 @@
 \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) &=