# New URL for NEMO forge! http://forge.nemo-ocean.eu

Since March 2022 along with NEMO 4.2 release, the code development moved to a self-hosted GitLab.
This present forge is now archived and remained online for history.
Changeset 10544 – NEMO

# Changeset 10544

Ignore:
Timestamp:
2019-01-18T14:20:35+01:00 (4 years ago)
Message:

Fixes for LaTeX compilation of NEMO manual

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

Unmodified
Removed
• ## NEMO/trunk/doc/latex/NEMO/main/NEMO_manual.sty

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

 r10502 the TEOS-10 rational function approximation for hydrographic data analysis \citep{TEOS10}. A key point is that conservative state variables are used: Absolute Salinity (unit: g/kg, notation: $S_A$) and Conservative Temperature (unit: \degC, notation: $\Theta$). Absolute Salinity (unit: g/kg, notation: $S_A$) and Conservative Temperature (unit: \deg{C}, notation: $\Theta$). The pressure in decibars is approximated by the depth in meters. 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 where $\vect U^\ast = \lt( u^\ast,v^\ast,w^\ast \rt)$ is a non-divergent, eddy-induced transport velocity. This velocity field is defined by: $\begin{gather} % \label{eq:PE_eiv} u^\ast &= \frac{1}{e_3} \pd[]{k} \lt( A^{eiv} \; \tilde{r}_1 \rt) \\ v^\ast &= \frac{1}{e_3} \pd[]{k} \lt( A^{eiv} \; \tilde{r}_2 \rt) \\ w^\ast &= - \frac{1}{e_1 e_2} \lt[ \pd[]{i} \lt( A^{eiv} \; e_2 \, \tilde{r}_1 \rt) u^\ast = \frac{1}{e_3} \pd[]{k} \lt( A^{eiv} \; \tilde{r}_1 \rt) \\ v^\ast = \frac{1}{e_3} \pd[]{k} \lt( A^{eiv} \; \tilde{r}_2 \rt) \\ w^\ast = - \frac{1}{e_1 e_2} \lt[ \pd[]{i} \lt( A^{eiv} \; e_2 \, \tilde{r}_1 \rt) + \pd[]{j} \lt( A^{eiv} \; e_1 \, \tilde{r}_2 \rt) \rt]$ \end{gather} where $A^{eiv}$ is the eddy induced velocity coefficient (or equivalently the isoneutral thickness diffusivity coefficient),
• ## NEMO/trunk/doc/latex/NEMO/subfiles/chap_model_basics_zstar.tex

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

 r10496 After the presentation of the continuous equations (\autoref{chap:PE}), the following chapters refer to specific terms of the equations each associated with a group of modules (\autoref{tab:chap}). (\autoref{tab:chapters}). %--------------------------------------------------TABLE--------------------------------------------------
Note: See TracChangeset for help on using the changeset viewer.