Ignore:
Timestamp:
2019-10-14T14:53:52+02:00 (13 months ago)
Author:
nicolasmartin
Message:

Macros renaming

File:
1 edited

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  • NEMO/trunk/doc/latex/NEMO/subfiles/chap_DYN.tex

    r11690 r11693  
    6767Furthermore, the tendency terms associated with the 2D barotropic vorticity balance (when \texttt{trdvor?} is defined) 
    6868can be derived from the 3D terms. 
    69 \gmcomment{STEVEN: not quite sure I've got the sense of the last sentence. does 
    70 MISC correspond to "extracting tendency terms" or "vorticity balance"?} 
     69\cmtgm{STEVEN: not quite sure I've got the sense of the last sentence. 
     70  Does MISC correspond to "extracting tendency terms" or "vorticity balance"?} 
    7171 
    7272%% ================================================================================================= 
     
    153153as changes in the divergence of the barotropic transport are absorbed into the change of the level thicknesses, 
    154154re-orientated downward. 
    155 \gmcomment{not sure of this...  to be modified with the change in emp setting} 
     155\cmtgm{not sure of this...  to be modified with the change in emp setting} 
    156156In the case of a linear free surface, the time derivative in \autoref{eq:DYN_wzv} disappears. 
    157157The upper boundary condition applies at a fixed level $z=0$. 
     
    287287$u$ and $v$ are located at different grid points, 
    288288a price worth paying to avoid a double averaging in the pressure gradient term as in the $B$-grid. 
    289 \gmcomment{ To circumvent this, Adcroft (ADD REF HERE) 
     289\cmtgm{ To circumvent this, Adcroft (ADD REF HERE) 
    290290Nevertheless, this technique strongly distort the phase and group velocity of Rossby waves....} 
    291291 
     
    516516In the vertical, the centred $2^{nd}$ order evaluation of the advection is preferred, \ie\ $u_{uw}^{ubs}$ and 
    517517$u_{vw}^{ubs}$ in \autoref{eq:DYN_adv_cen2} are used. 
    518 UBS is diffusive and is associated with vertical mixing of momentum. \gmcomment{ gm  pursue the 
     518UBS is diffusive and is associated with vertical mixing of momentum. \cmtgm{ gm  pursue the 
    519519sentence:Since vertical mixing of momentum is a source term of the TKE equation...  } 
    520520 
     
    534534there is also the possibility of using a $4^{th}$ order evaluation of the advective velocity as in ROMS. 
    535535This is an error and should be suppressed soon. 
    536 \gmcomment{action :  this have to be done} 
     536\cmtgm{action :  this have to be done} 
    537537 
    538538%% ================================================================================================= 
     
    915915it is still significant as shown by \citet{levier.treguier.ea_rpt07} in the case of an analytical barotropic Kelvin wave. 
    916916 
    917 \gmcomment{               %%% copy from griffies Book 
     917\cmtgm{               %%% copy from griffies Book 
    918918 
    919919\textbf{title: Time stepping the barotropic system } 
     
    10431043 
    10441044%% gm %%======>>>>   given here the discrete eqs provided to the solver 
    1045 \gmcomment{               %%% copy from chap-model basics 
     1045\cmtgm{               %%% copy from chap-model basics 
    10461046  \[ 
    10471047    % \label{eq:DYN_spg_flt} 
     
    10541054  and $\mathrm {\mathbf M}$ represents the collected contributions of the Coriolis, hydrostatic pressure gradient, 
    10551055  non-linear and viscous terms in \autoref{eq:MB_dyn}. 
    1056 }   %end gmcomment 
     1056}   %end cmtgm 
    10571057 
    10581058Note that in the linear free surface formulation (\texttt{vvl?} not defined), 
     
    10821082no slip or partial slip boundary conditions are applied according to the user's choice (see \autoref{chap:LBC}). 
    10831083 
    1084 \gmcomment{ 
     1084\cmtgm{ 
    10851085  Hyperviscous operators are frequently used in the simulation of turbulent flows to 
    10861086  control the dissipation of unresolved small scale features. 
     
    11831183the first derivative term normal to the coast depends on the free or no-slip lateral boundary conditions chosen, 
    11841184while the third derivative terms normal to the coast are set to zero (see \autoref{chap:LBC}). 
    1185 \gmcomment{add a remark on the the change in the position of the coefficient} 
     1185\cmtgm{add a remark on the the change in the position of the coefficient} 
    11861186 
    11871187%% ================================================================================================= 
     
    12521252the snow-ice mass is taken into account when computing the surface pressure gradient. 
    12531253 
    1254 \gmcomment{ missing : the lateral boundary condition !!!   another external forcing 
     1254\cmtgm{ missing : the lateral boundary condition !!!   another external forcing 
    12551255 } 
    12561256 
     
    15961596and only array swapping and Asselin filtering is done in \mdl{dynnxt}. 
    15971597 
    1598 \onlyinsubfile{\input{../../global/epilogue}} 
     1598\subinc{\input{../../global/epilogue}} 
    15991599 
    16001600\end{document} 
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