Changeset 12928 for NEMO/branches/2019/dev_r11078_OSMOSIS_IMMERSE_Nurser/doc/latex/NEMO/subfiles/chap_DYN.tex
- Timestamp:
- 2020-05-14T21:46:00+02:00 (4 years ago)
- Location:
- NEMO/branches/2019/dev_r11078_OSMOSIS_IMMERSE_Nurser
- Files:
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- 2 edited
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NEMO/branches/2019/dev_r11078_OSMOSIS_IMMERSE_Nurser
- Property svn:externals
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old new 6 6 ^/vendors/FCM@HEAD ext/FCM 7 7 ^/vendors/IOIPSL@HEAD ext/IOIPSL 8 9 # SETTE 10 ^/utils/CI/sette@HEAD sette
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- Property svn:externals
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NEMO/branches/2019/dev_r11078_OSMOSIS_IMMERSE_Nurser/doc/latex/NEMO/subfiles/chap_DYN.tex
r12178 r12928 67 67 Furthermore, the tendency terms associated with the 2D barotropic vorticity balance (when \texttt{trdvor?} is defined) 68 68 can be derived from the 3D terms. 69 \ gmcomment{STEVEN: not quite sure I've got the sense of the last sentence. does70 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"?} 71 71 72 72 %% ================================================================================================= … … 153 153 as changes in the divergence of the barotropic transport are absorbed into the change of the level thicknesses, 154 154 re-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} 156 156 In the case of a linear free surface, the time derivative in \autoref{eq:DYN_wzv} disappears. 157 157 The upper boundary condition applies at a fixed level $z=0$. … … 287 287 $u$ and $v$ are located at different grid points, 288 288 a 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) 290 290 Nevertheless, this technique strongly distort the phase and group velocity of Rossby waves....} 291 291 … … 311 311 \begin{figure}[!ht] 312 312 \centering 313 \includegraphics[width=0.66\textwidth]{ Fig_DYN_een_triad}313 \includegraphics[width=0.66\textwidth]{DYN_een_triad} 314 314 \caption[Triads used in the energy and enstrophy conserving scheme (EEN)]{ 315 315 Triads used in the energy and enstrophy conserving scheme (EEN) for … … 516 516 In the vertical, the centred $2^{nd}$ order evaluation of the advection is preferred, \ie\ $u_{uw}^{ubs}$ and 517 517 $u_{vw}^{ubs}$ in \autoref{eq:DYN_adv_cen2} are used. 518 UBS is diffusive and is associated with vertical mixing of momentum. \ gmcomment{ gm pursue the518 UBS is diffusive and is associated with vertical mixing of momentum. \cmtgm{ gm pursue the 519 519 sentence:Since vertical mixing of momentum is a source term of the TKE equation... } 520 520 … … 534 534 there is also the possibility of using a $4^{th}$ order evaluation of the advective velocity as in ROMS. 535 535 This is an error and should be suppressed soon. 536 \ gmcomment{action : this have to be done}536 \cmtgm{action : this have to be done} 537 537 538 538 %% ================================================================================================= … … 846 846 \begin{figure}[!t] 847 847 \centering 848 \includegraphics[width=0.66\textwidth]{ Fig_DYN_dynspg_ts}848 \includegraphics[width=0.66\textwidth]{DYN_dynspg_ts} 849 849 \caption[Split-explicit time stepping scheme for the external and internal modes]{ 850 850 Schematic of the split-explicit time stepping scheme for the external and internal modes. … … 915 915 it is still significant as shown by \citet{levier.treguier.ea_rpt07} in the case of an analytical barotropic Kelvin wave. 916 916 917 \ gmcomment{ %%% copy from griffies Book917 \cmtgm{ %%% copy from griffies Book 918 918 919 919 \textbf{title: Time stepping the barotropic system } … … 1043 1043 1044 1044 %% gm %%======>>>> given here the discrete eqs provided to the solver 1045 \ gmcomment{ %%% copy from chap-model basics1045 \cmtgm{ %%% copy from chap-model basics 1046 1046 \[ 1047 1047 % \label{eq:DYN_spg_flt} … … 1054 1054 and $\mathrm {\mathbf M}$ represents the collected contributions of the Coriolis, hydrostatic pressure gradient, 1055 1055 non-linear and viscous terms in \autoref{eq:MB_dyn}. 1056 } %end gmcomment1056 } %end cmtgm 1057 1057 1058 1058 Note that in the linear free surface formulation (\texttt{vvl?} not defined), … … 1082 1082 no slip or partial slip boundary conditions are applied according to the user's choice (see \autoref{chap:LBC}). 1083 1083 1084 \ gmcomment{1084 \cmtgm{ 1085 1085 Hyperviscous operators are frequently used in the simulation of turbulent flows to 1086 1086 control the dissipation of unresolved small scale features. … … 1183 1183 the first derivative term normal to the coast depends on the free or no-slip lateral boundary conditions chosen, 1184 1184 while 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} 1186 1186 1187 1187 %% ================================================================================================= … … 1252 1252 the snow-ice mass is taken into account when computing the surface pressure gradient. 1253 1253 1254 \ gmcomment{ missing : the lateral boundary condition !!! another external forcing1254 \cmtgm{ missing : the lateral boundary condition !!! another external forcing 1255 1255 } 1256 1256 … … 1480 1480 \begin{figure}[!ht] 1481 1481 \centering 1482 \includegraphics[width=0.66\textwidth]{ Fig_WAD_dynhpg}1482 \includegraphics[width=0.66\textwidth]{DYN_WAD_dynhpg} 1483 1483 \caption[Combinations controlling the limiting of the horizontal pressure gradient in 1484 1484 wetting and drying regimes]{ … … 1596 1596 and only array swapping and Asselin filtering is done in \mdl{dynnxt}. 1597 1597 1598 \ onlyinsubfile{\input{../../global/epilogue}}1598 \subinc{\input{../../global/epilogue}} 1599 1599 1600 1600 \end{document}
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