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Commit a3742987 authored by Sibylle Techene's avatar Sibylle Techene
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Update chap_DYN.tex

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......@@ -802,8 +802,8 @@ The pressure gradient due to ocean load is computed using the expression \autore
Options are defined through the \nam{dyn_spg}{dyn\_spg} namelist variables.
The surface pressure gradient term is related to the representation of the free surface (\autoref{sec:MB_hor_pg}).
The main distinction is between the fixed volume case (linear free surface, \ie\ \np[=.true.]{ln_linssh}{ln\_linssh}) and
the variable volume case (nonlinear free surface, \np[=.false.]{ln_linssh}{ln\_linssh}).
The main distinction is between the fixed volume case (linear free surface, \ie\ with the inclusion of \key{linssh}) and
the variable volume case (nonlinear free surface, \key{qco}).
In the linear free surface case (\autoref{subsec:MB_free_surface})
the vertical scale factors $e_{3}$ are fixed in time,
while they are time-dependent in the nonlinear case (\autoref{subsec:MB_free_surface}).
......@@ -832,6 +832,8 @@ is thus simply given by :
\right.
\end{equation}
Note that this option is not yet compatible with RK3 time-stepping.
%% =================================================================================================
\subsection[Split-explicit free surface (\forcode{ln_dynspg_ts})]{Split-explicit free surface (\protect\np{ln_dynspg_ts}{ln\_dynspg\_ts})}
\label{subsec:DYN_spg_ts}
......
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