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/apdx_algos.tex

    r11690 r11693  
    311311\begin{figure}[!ht] 
    312312  \centering 
    313   \includegraphics[width=0.66\textwidth]{ALGOS_ISO_triad} 
     313  %\includegraphics[width=0.66\textwidth]{ALGOS_ISO_triad} 
    314314  \caption[Triads used in the Griffies's like iso-neutral diffision scheme for 
    315315    $u$- and $w$-components)]{ 
     
    461461where $A_{e}$ is the eddy induced velocity coefficient, 
    462462and $r_i$ and $r_j$ the slopes between the iso-neutral and the geopotential surfaces. 
    463 %%gm wrong: to be modified with 2 2D streamfunctions 
     463\cmtgm{Wrong: to be modified with 2 2D streamfunctions} 
    464464In other words, the eddy induced velocity can be derived from a vector streamfuntion, $\phi$, 
    465465which is given by $\phi = A_e\,\textbf{r}$ as $\textbf{U}^*  = \textbf{k} \times \nabla \phi$. 
    466 %%end gm 
    467466 
    468467A traditional way to implement this additional advection is to add it to the eulerian velocity prior to 
     
    822821\ie\ the variance of the tracer is preserved by the discretisation of the skew fluxes. 
    823822 
    824 \onlyinsubfile{\input{../../global/epilogue}} 
     823\subinc{\input{../../global/epilogue}} 
    825824 
    826825\end{document} 
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