Changeset 14526 for NEMO/trunk/doc/latex/NEMO/subfiles/chap_SBC.tex

Timestamp:

2021-02-22T17:37:38+01:00 (3 years ago)

Author:

nicolasmartin

Message:

Modify \nlst LaTeX macro for better efficienty
Only one line is needed now to include the highlighted source code, the caption and the cross-reference

\newcommand{\nlst}[1]{
   \begin{listing}
      \newmintedfile{fortran}{../../../namelists/#1}
      \caption{\forcode{&#1}}
      \label{lst:#1}
   \end{listing}
}

File:

• NEMO/trunk/doc/latex/NEMO/subfiles/chap_SBC.tex (modified) (13 diffs)

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

@@ -25 +25 @@
 \clearpage
 
-\begin{listing}
-  \nlst{namsbc}
-  \caption{\forcode{&namsbc}}
-  \label{lst:namsbc}
-\end{listing}
+\nlst{namsbc}
 
 The ocean needs seven fields as surface boundary condition:
@@ -438 +434 @@
 \label{subsec:SBC_SAS}
 
-\begin{listing}
-  \nlst{namsbc_sas}
-  \caption{\forcode{&namsbc_sas}}
-  \label{lst:namsbc_sas}
-\end{listing}
+\nlst{namsbc_sas}
 
 In some circumstances, it may be useful to avoid calculating the 3D temperature,
@@ -503 +495 @@
 % parameterization'' (i.e NCAR, COARE, ECMWF...)
 
-\begin{listing}
-  \nlst{namsbc_flx}
-  \caption{\forcode{&namsbc_flx}}
-  \label{lst:namsbc_flx}
-\end{listing}
+\nlst{namsbc_flx}
 
 In the flux formulation (\np[=.true.]{ln_flx}{ln\_flx}),
@@ -525 +513 @@
 % L. Brodeau, December 2019... %
 
-\begin{listing}
-  \nlst{namsbc_blk}
-  \caption{\forcode{&namsbc_blk}}
-  \label{lst:namsbc_blk}
-\end{listing}
+\nlst{namsbc_blk}
 
 If the bulk formulation is selected (\np[=.true.]{ln_blk}{ln\_blk}), the air-sea
@@ -884 +868 @@
 \label{sec:SBC_cpl}
 
-\begin{listing}
-  \nlst{namsbc_cpl}
-  \caption{\forcode{&namsbc_cpl}}
-  \label{lst:namsbc_cpl}
-\end{listing}
+\nlst{namsbc_cpl}
 
 In the coupled formulation of the surface boundary condition,
@@ -920 +900 @@
 \label{sec:SBC_apr}
 
-\begin{listing}
-  \nlst{namsbc_apr}
-  \caption{\forcode{&namsbc_apr}}
-  \label{lst:namsbc_apr}
-\end{listing}
+\nlst{namsbc_apr}
 
 The optional atmospheric pressure can be used to force ocean and ice dynamics
@@ -956 +932 @@
 \label{sec:SBC_TDE}
 
-\begin{listing}
-  \nlst{nam_tide}
-  \caption{\forcode{&nam_tide}}
-  \label{lst:nam_tide}
-\end{listing}
+\nlst{nam_tide}
 
 \subsection{Tidal constituents}
@@ -1043 +1015 @@
 \label{sec:SBC_rnf}
 
-\begin{listing}
-  \nlst{namsbc_rnf}
-  \caption{\forcode{&namsbc_rnf}}
-  \label{lst:namsbc_rnf}
-\end{listing}
+\nlst{namsbc_rnf}
 
 %River runoff generally enters the ocean at a nonzero depth rather than through the surface.
@@ -1181 +1149 @@
 \label{sec:SBC_isf}
 
-\begin{listing}
-  \nlst{namisf}
-  \caption{\forcode{&namisf}}
-  \label{lst:namisf}
-\end{listing}
+\nlst{namisf}
 
 The namelist variable in \nam{isf}{isf}, \np{ln_isf}{ln\_isf}, controls the ice shelf interactions:
@@ -1491 +1455 @@
 \label{sec:SBC_ICB_icebergs}
 
-\begin{listing}
-  \nlst{namberg}
-  \caption{\forcode{&namberg}}
-  \label{lst:namberg}
-\end{listing}
+\nlst{namberg}
 
 Icebergs are modelled as lagrangian particles in \NEMO\ \citep{marsh.ivchenko.ea_GMD15}.
@@ -1564 +1524 @@
 \label{sec:SBC_wave}
 
-\begin{listing}
-  \nlst{namsbc_wave}
-  \caption{\forcode{&namsbc_wave}}
-  \label{lst:namsbc_wave}
-\end{listing}
+\nlst{namsbc_wave}
 
 Ocean waves represent the interface between the ocean and the atmosphere, so \NEMO\ is extended to incorporate
@@ -1818 +1774 @@
 \label{subsec:SBC_ssr}
 
-\begin{listing}
-  \nlst{namsbc_ssr}
-  \caption{\forcode{&namsbc_ssr}}
-  \label{lst:namsbc_ssr}
-\end{listing}
+\nlst{namsbc_ssr}
 
 Options are defined through the \nam{sbc_ssr}{sbc\_ssr} namelist variables.
@@ -1927 +1879 @@
 \label{subsec:SBC_fwb}
 
-\begin{listing}
-  \nlst{namsbc_fwb}
-  \caption{\forcode{&namsbc_fwb}}
-  \label{lst:namsbc_fwb}
-\end{listing}
+\nlst{namsbc_fwb}
 
 For global ocean simulations, it can be useful to introduce a control of the