Changeset 11693 for NEMO/trunk/doc/latex/NEMO/subfiles/apdx_algos.tex
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 20191014T14:53:52+02:00 (13 months ago)
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NEMO/trunk/doc/latex/NEMO/subfiles/apdx_algos.tex
r11690 r11693 311 311 \begin{figure}[!ht] 312 312 \centering 313 \includegraphics[width=0.66\textwidth]{ALGOS_ISO_triad}313 %\includegraphics[width=0.66\textwidth]{ALGOS_ISO_triad} 314 314 \caption[Triads used in the Griffies's like isoneutral diffision scheme for 315 315 $u$ and $w$components)]{ … … 461 461 where $A_{e}$ is the eddy induced velocity coefficient, 462 462 and $r_i$ and $r_j$ the slopes between the isoneutral and the geopotential surfaces. 463 %%gm wrong: to be modified with 2 2D streamfunctions 463 \cmtgm{Wrong: to be modified with 2 2D streamfunctions} 464 464 In other words, the eddy induced velocity can be derived from a vector streamfuntion, $\phi$, 465 465 which is given by $\phi = A_e\,\textbf{r}$ as $\textbf{U}^* = \textbf{k} \times \nabla \phi$. 466 %%end gm467 466 468 467 A traditional way to implement this additional advection is to add it to the eulerian velocity prior to … … 822 821 \ie\ the variance of the tracer is preserved by the discretisation of the skew fluxes. 823 822 824 \ onlyinsubfile{\input{../../global/epilogue}}823 \subinc{\input{../../global/epilogue}} 825 824 826 825 \end{document}
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