Changeset 11683

Timestamp:

2019-10-11T00:16:09+02:00 (4 years ago)

Author:

agn

Message:

Monday morning

File:

• NEMO/trunk/doc/latex/NEMO/subfiles/chap_ZDF.tex (modified) (4 diffs)

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

@@ -550 +550 @@
 Most of the namelist options refer to how to specify the Stokes
 surface drift and penetration depth. There are three options:
-\begin{enumerate}
-  \item \np{nn\_osm\_wave=0}. Default value in \texttt{namelist\_ref}. In this case the Stokes drift is
+\begin{description}
+  \item \np{nn\_osm\_wave=0} Default value in \texttt{namelist\_ref}. In this case the Stokes drift is
       assumed to be parallel to the surface wind stress, with
       magnitude consistent with a constant turbulent Langmuir number
@@ -560 +560 @@
       of \SI{5 m}.
  
-  \item \np{nn\_osm\_wave=1}. In this case the Stokes drift is
+  \item \np{nn\_osm\_wave=1} In this case the Stokes drift is
       assumed to be parallel to the surface wind stress, with
       magnitude as in the classical Pierson-Moskowitz wind-sea
@@ -567 +567 @@
       depth, following the approach set out in Breivik(XXxx)
  
-    \item \np{nn\_osm\_wave=2}. In this case the Stokes drift is
+    \item \np{nn\_osm\_wave=2} In this case the Stokes drift is
       taken from  ECMWF wave model output, though only the component parallel
       to the wind stress is retained. Significant wave height and
@@ -573 +573 @@
       depth, following the approach set out in Breivik(XXxx).
 
-    \end{enumerate}
+    \end{description}
 
     Others refer to the treatment of diffusion and viscosity beneath
     the surface boundary layer:
-\begin{enumerate}
-   \item \np{ln\_kpprimix}.  Default is \np{.true.}. Switches on KPP-style Ri #-dependent
+\begin{description}
+   \item \np{ln\_kpprimix}  Default is \np{.true.}. Switches on KPP-style Ri \#-dependent
      mixing below the surface boundary layer. If this is set
      \np{.true.}  the following variable settings are honoured:
-    \item \np{rn\_riinfty}. Critical value of local Ri # below which
+    \item \np{rn\_riinfty} Critical value of local Ri \# below which
       shear instability increases vertical mixing from background value.
-    \item \np{rn\_difri}. Critical value of local Ri # below which
-      shear instability increases vertical mixing from background value.
-  \end{enumerate}
-  and the last to diagnostic outputs:
-  \begin{list}
-    \item \np{ln\_dia\_osm}. Default is \np{.false.}; allows XIOS output of OSMOSIS internal fields.
-  \end{list}
-
-    
-    Obsolete namelist parameters include:
-  \begin{enumerate}
-   \item \np{ln\_use\_osm\_la}. With \np{nn\_osm\_wave=0},
+    \item \np{rn\_difri} Maximum value of Ri \#-dependent mixing at $\mathrm{Ri}=0$.
+    \item \np{ln\_convmix} If \texttt{.true.} then, where water column is unstable, specify
+       diffusivity equal to \np{rn\_dif\_conv} (default value is 1 ms$^{-2}$). 
+ \end{description}
+ Diagnostic output is controlled by:
+  \begin{description}
+    \item \np{ln\_dia\_osm} Default is \np{.false.}; allows XIOS output of OSMOSIS internal fields.
+  \end{description}
+Obsolete namelist parameters include:
+\begin{description}
+   \item \np{ln\_use\_osm\_la} With \np{nn\_osm\_wave=0},
       \np{rn\_osm\_dstokes} is always used to specify the Stokes
       penetration depth.
-
-    \item \np{nn\_ave}. Choice of averaging method for KPP-style Ri#
+   \item \np{nn\_ave} Choice of averaging method for KPP-style Ri#
       mixing. Not taken account of.
- 
-     \item \np{rn\_osm\_hbl0}
-     \item \np{ln\_dia\_osm}
-      \end{enumerate}
+   \item \np{rn\_osm\_hbl0} Depth of initial boundary layer is now set
+     by a desnity criterion similar to that used in  
+\end{description}
 
 \subsubsection{Summary}