Index: NEMO/trunk/doc/latex/NEMO/subfiles/chap_DYN.tex
===================================================================
--- NEMO/trunk/doc/latex/NEMO/subfiles/chap_DYN.tex	(revision 11690)
+++ NEMO/trunk/doc/latex/NEMO/subfiles/chap_DYN.tex	(revision 11693)
@@ -67,6 +67,6 @@
 Furthermore, the tendency terms associated with the 2D barotropic vorticity balance (when \texttt{trdvor?} is defined)
 can be derived from the 3D terms.
-\gmcomment{STEVEN: not quite sure I've got the sense of the last sentence. does
-MISC correspond to "extracting tendency terms" or "vorticity balance"?}
+\cmtgm{STEVEN: not quite sure I've got the sense of the last sentence.
+  Does MISC correspond to "extracting tendency terms" or "vorticity balance"?}
 
 %% =================================================================================================
@@ -153,5 +153,5 @@
 as changes in the divergence of the barotropic transport are absorbed into the change of the level thicknesses,
 re-orientated downward.
-\gmcomment{not sure of this...  to be modified with the change in emp setting}
+\cmtgm{not sure of this...  to be modified with the change in emp setting}
 In the case of a linear free surface, the time derivative in \autoref{eq:DYN_wzv} disappears.
 The upper boundary condition applies at a fixed level $z=0$.
@@ -287,5 +287,5 @@
 $u$ and $v$ are located at different grid points,
 a price worth paying to avoid a double averaging in the pressure gradient term as in the $B$-grid.
-\gmcomment{ To circumvent this, Adcroft (ADD REF HERE)
+\cmtgm{ To circumvent this, Adcroft (ADD REF HERE)
 Nevertheless, this technique strongly distort the phase and group velocity of Rossby waves....}
 
@@ -516,5 +516,5 @@
 In the vertical, the centred $2^{nd}$ order evaluation of the advection is preferred, \ie\ $u_{uw}^{ubs}$ and
 $u_{vw}^{ubs}$ in \autoref{eq:DYN_adv_cen2} are used.
-UBS is diffusive and is associated with vertical mixing of momentum. \gmcomment{ gm  pursue the
+UBS is diffusive and is associated with vertical mixing of momentum. \cmtgm{ gm  pursue the
 sentence:Since vertical mixing of momentum is a source term of the TKE equation...  }
 
@@ -534,5 +534,5 @@
 there is also the possibility of using a $4^{th}$ order evaluation of the advective velocity as in ROMS.
 This is an error and should be suppressed soon.
-\gmcomment{action :  this have to be done}
+\cmtgm{action :  this have to be done}
 
 %% =================================================================================================
@@ -915,5 +915,5 @@
 it is still significant as shown by \citet{levier.treguier.ea_rpt07} in the case of an analytical barotropic Kelvin wave.
 
-\gmcomment{               %%% copy from griffies Book
+\cmtgm{               %%% copy from griffies Book
 
 \textbf{title: Time stepping the barotropic system }
@@ -1043,5 +1043,5 @@
 
 %% gm %%======>>>>   given here the discrete eqs provided to the solver
-\gmcomment{               %%% copy from chap-model basics
+\cmtgm{               %%% copy from chap-model basics
   \[
     % \label{eq:DYN_spg_flt}
@@ -1054,5 +1054,5 @@
   and $\mathrm {\mathbf M}$ represents the collected contributions of the Coriolis, hydrostatic pressure gradient,
   non-linear and viscous terms in \autoref{eq:MB_dyn}.
-}   %end gmcomment
+}   %end cmtgm
 
 Note that in the linear free surface formulation (\texttt{vvl?} not defined),
@@ -1082,5 +1082,5 @@
 no slip or partial slip boundary conditions are applied according to the user's choice (see \autoref{chap:LBC}).
 
-\gmcomment{
+\cmtgm{
   Hyperviscous operators are frequently used in the simulation of turbulent flows to
   control the dissipation of unresolved small scale features.
@@ -1183,5 +1183,5 @@
 the first derivative term normal to the coast depends on the free or no-slip lateral boundary conditions chosen,
 while the third derivative terms normal to the coast are set to zero (see \autoref{chap:LBC}).
-\gmcomment{add a remark on the the change in the position of the coefficient}
+\cmtgm{add a remark on the the change in the position of the coefficient}
 
 %% =================================================================================================
@@ -1252,5 +1252,5 @@
 the snow-ice mass is taken into account when computing the surface pressure gradient.
 
-\gmcomment{ missing : the lateral boundary condition !!!   another external forcing
+\cmtgm{ missing : the lateral boundary condition !!!   another external forcing
  }
 
@@ -1596,5 +1596,5 @@
 and only array swapping and Asselin filtering is done in \mdl{dynnxt}.
 
-\onlyinsubfile{\input{../../global/epilogue}}
+\subinc{\input{../../global/epilogue}}
 
 \end{document}
