# Changeset 11693 for NEMO/trunk/doc/latex/NEMO/subfiles/apdx_algos.tex

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

Macros renaming

File:
1 edited

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Removed
• ## NEMO/trunk/doc/latex/NEMO/subfiles/apdx_algos.tex

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