Changeset 14530 for NEMO/trunk/doc/latex/NEMO/subfiles/chap_SBC.tex

Timestamp:

2021-02-22T21:19:07+01:00 (3 years ago)

Author:

nicolasmartin

Message:

Revert commit 14526, can't use verbatim envs in macro

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