Changeset 10544


Ignore:
Timestamp:
2019-01-18T14:20:35+01:00 (18 months ago)
Author:
nicolasmartin
Message:

Fixes for LaTeX compilation of NEMO manual

Location:
NEMO/trunk/doc/latex/NEMO
Files:
5 edited

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  • NEMO/trunk/doc/latex/NEMO/main/NEMO_manual.sty

    r10442 r10544  
    135135 
    136136%% Maths 
     137\newcommand{\lt}{\left} 
     138\newcommand{\rt}{\right} 
    137139\newcommand{\vect}[1]{\ensuremath{\mathbf{#1}}} 
    138140\newcommand{\pd}[2][]{\ensuremath{\frac{\partial #1}{\partial #2}}} 
  • NEMO/trunk/doc/latex/NEMO/subfiles/chap_TRA.tex

    r10502 r10544  
    12191219  the TEOS-10 rational function approximation for hydrographic data analysis \citep{TEOS10}. 
    12201220  A key point is that conservative state variables are used: 
    1221   Absolute Salinity (unit: g/kg, notation: $S_A$) and Conservative Temperature (unit: \degC, notation: $\Theta$). 
     1221  Absolute Salinity (unit: g/kg, notation: $S_A$) and Conservative Temperature (unit: \deg{C}, notation: $\Theta$). 
    12221222  The pressure in decibars is approximated by the depth in meters. 
    12231223  With TEOS10, the specific heat capacity of sea water, $C_p$, is a constant. 
  • NEMO/trunk/doc/latex/NEMO/subfiles/chap_model_basics.tex

    r10501 r10544  
    10951095where $ \vect U^\ast = \lt( u^\ast,v^\ast,w^\ast \rt)$ is a non-divergent, 
    10961096eddy-induced transport velocity. This velocity field is defined by: 
    1097 \[ 
     1097\begin{gather} 
    10981098  % \label{eq:PE_eiv} 
    1099   u^\ast &=   \frac{1}{e_3}            \pd[]{k} \lt( A^{eiv} \;        \tilde{r}_1 \rt) \\ 
    1100   v^\ast &=   \frac{1}{e_3}            \pd[]{k} \lt( A^{eiv} \;        \tilde{r}_2 \rt) \\ 
    1101   w^\ast &= - \frac{1}{e_1 e_2} \lt[   \pd[]{i} \lt( A^{eiv} \; e_2 \, \tilde{r}_1 \rt) 
     1099  u^\ast =   \frac{1}{e_3}            \pd[]{k} \lt( A^{eiv} \;        \tilde{r}_1 \rt) \\ 
     1100  v^\ast =   \frac{1}{e_3}            \pd[]{k} \lt( A^{eiv} \;        \tilde{r}_2 \rt) \\ 
     1101  w^\ast = - \frac{1}{e_1 e_2} \lt[   \pd[]{i} \lt( A^{eiv} \; e_2 \, \tilde{r}_1 \rt) 
    11021102                                     + \pd[]{j} \lt( A^{eiv} \; e_1 \, \tilde{r}_2 \rt) \rt] 
    1103 \] 
     1103\end{gather} 
    11041104where $A^{eiv}$ is the eddy induced velocity coefficient 
    11051105(or equivalently the isoneutral thickness diffusivity coefficient), 
  • NEMO/trunk/doc/latex/NEMO/subfiles/chap_model_basics_zstar.tex

    r10442 r10544  
    8989which imposes a very small time step when an explicit time stepping is used. 
    9090Two methods are proposed to allow a longer time step for the three-dimensional equations: 
    91 the filtered free surface, which is a modification of the continuous equations (see \autoref{eq:PE_flt}), 
     91the filtered free surface, which is a modification of the continuous equations %(see \autoref{eq:PE_flt}), 
    9292and the split-explicit free surface described below. 
    9393The extra term introduced in the filtered method is calculated implicitly, 
  • NEMO/trunk/doc/latex/NEMO/subfiles/introduction.tex

    r10496 r10544  
    165165After the presentation of the continuous equations (\autoref{chap:PE}), 
    166166the following chapters refer to specific terms of the equations each associated with a group of modules  
    167 (\autoref{tab:chap}). 
     167(\autoref{tab:chapters}). 
    168168 
    169169%--------------------------------------------------TABLE-------------------------------------------------- 
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