Changeset 11954 for NEMO/branches/2019/dev_r11613_ENHANCE-04_namelists_as_internalfiles/doc/latex/NEMO/subfiles/apdx_algos.tex

Timestamp:

2019-11-22T17:15:18+01:00 (4 years ago)

Author:

acc

Message:

Branch 2019/dev_r11613_ENHANCE-04_namelists_as_internalfiles. Merge in trunk changes up to 11943 in preparation for end of year merge

File:

• NEMO/branches/2019/dev_r11613_ENHANCE-04_namelists_as_internalfiles/doc/latex/NEMO/subfiles/apdx_algos.tex (modified) (3 diffs)

NEMO/branches/2019/dev_r11613_ENHANCE-04_namelists_as_internalfiles/doc/latex/NEMO/subfiles/apdx_algos.tex

@@ -311 +311 @@
 \begin{figure}[!ht]
   \centering
-  \includegraphics[width=0.66\textwidth]{Fig_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)]{
@@ -461 +461 @@
 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
@@ -822 +821 @@
 \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}