Merge branch 'manual_revision_2022' of forge.nemo-ocean.eu:nemo/nemo into manual_revision_2022

doc/latex/NEMO/main/introduction.tex

@@ -73,8 +73,6 @@ Interactive coupling to Atmospheric models is possible via the \OASIS\ coupler.
 Two-way nesting is also available through an interface to the \AGRIF\ package,
 \ie\ \textbf{A}daptative \textbf{G}rid \textbf{R}efinement in \textbf{F}ortran
 \citep{debreu.vouland.ea_CG08}.
-The interface code for coupling to an alternative sea ice model (\CICE) has now been upgraded so that
-it works for both global and regional domains.
 \item [\nameref{chap:LBC}] presents the \textbf{L}ateral
 \textbf{B}oun\textbf{D}ar\textbf{Y} \textbf{C}onditions.
 Global configurations of the model make use of the ORCA tripolar grid,

doc/latex/NEMO/subfiles/chap_DYN.tex

@@ -1223,7 +1223,7 @@ the atmospheric pressure is taken into account when computing the surface pressu
 (2) When \np[=.true.]{ln_tide_pot}{ln\_tide\_pot} and \np[=.true.]{ln_tide}{ln\_tide} (see \autoref{sec:SBC_TDE}),
 the tidal potential is taken into account when computing the surface pressure gradient.
 
-(3) When \np[=2]{nn_ice_embd}{nn\_ice\_embd} and LIM or CICE is used
+(3) When \np[=2]{nn_ice_embd}{nn\_ice\_embd} and SI3 is used
 (\ie\ when the sea-ice is embedded in the ocean),
 the snow-ice mass is taken into account when computing the surface pressure gradient.
 

doc/latex/NEMO/subfiles/introduction.tex

@@ -69,9 +69,6 @@ a biogeochemistry model (PISCES).
 Interactive coupling to Atmospheric models is possible via the \href{https://portal.enes.org/oasis}{OASIS coupler}.
 Two-way nesting is also available through an interface to the AGRIF package
 (Adaptative Grid Refinement in \fortran) \citep{debreu.vouland.ea_CG08}.
-% Needs to be reviewed
-%The interface code for coupling to an alternative sea ice model (CICE, \citet{Hunke2008}) has now been upgraded so
-%that it works for both global and regional domains, although AGRIF is still not available.
 
 Other model characteristics are the lateral boundary conditions (\autoref{chap:LBC}).
 Global configurations of the model make use of the ORCA tripolar grid, with special north fold boundary condition.