Changeset 11524

Timestamp:

2019-09-10T16:09:48+02:00 (5 years ago)

Author:

nicolasmartin

Message:

Bugfixes

Location:

NEMO/trunk/doc/latex

Files:

• NEMO/subfiles/chap_TRA.tex (modified) (5 diffs)
• global/document.tex (modified) (1 diff)

NEMO/trunk/doc/latex/NEMO/subfiles/chap_TRA.tex

@@ -139 +139 @@
 two quantities that are not correlated \citep{roullet.madec_JGR00, griffies.pacanowski.ea_MWR01, campin.adcroft.ea_OM04}.
 
-The velocity field that appears in (\autoref{eq:tra_adv} is 
+The velocity field that appears in (\autoref{eq:tra_adv} is
 the centred (\textit{now}) \textit{effective} ocean velocity, \ie\ the \textit{eulerian} velocity
 (see \autoref{chap:DYN}) plus the eddy induced velocity (\textit{eiv}) and/or
@@ -471 +471 @@
 \item[\np{ln\_traldf\_lap}\forcode{ = .true.}:]
   a laplacian operator is selected.
-  This harmonic operator takes the following expression:  $\mathpzc{L}(T) = \nabla \cdot A_{ht} \; \nabla T $,
+  This harmonic operator takes the following expression:  $\mathcal{L}(T) = \nabla \cdot A_{ht} \; \nabla T $,
   where the gradient operates along the selected direction (see \autoref{subsec:TRA_ldf_dir}),
   and $A_{ht}$ is the eddy diffusivity coefficient expressed in $m^2/s$ (see \autoref{chap:LDF}).
@@ -477 +477 @@
   a bilaplacian operator is selected.
   This biharmonic operator takes the following expression:
-  $\mathpzc{B} = - \mathpzc{L}(\mathpzc{L}(T)) = - \nabla \cdot b \nabla (\nabla \cdot b \nabla T)$
+  $\mathcal{B} = - \mathcal{L}(\mathcal{L}(T)) = - \nabla \cdot b \nabla (\nabla \cdot b \nabla T)$
   where the gradient operats along the selected direction,
   and $b^2 = B_{ht}$ is the eddy diffusivity coefficient expressed in $m^4/s$ (see \autoref{chap:LDF}).
@@ -534 +534 @@
 where zero diffusive fluxes is assumed across solid boundaries,
 first (and third in bilaplacian case) horizontal tracer derivative are masked.
-It is implemented in the \rou{tra\_ldf\_lap} subroutine found in the \mdl{traldf\_lap\_blp}} module.
+It is implemented in the \rou{tra\_ldf\_lap} subroutine found in the \mdl{traldf\_lap\_blp} module.
 The module also contains \rou{tra\_ldf\_blp}, the subroutine calling twice \rou{tra\_ldf\_lap} in order to
 compute the iso-level bilaplacian operator.
@@ -1217 +1217 @@
 density in the World Ocean varies by no more than 2$\%$ from that value \citep{gill_bk82}.
 
-Options which control the EOS used are defined through the \ngn{nameos} namelist variables.
+Options which control the EOS used are defined through the \nam{eos} namelist variables.
 
 \begin{description}

NEMO/trunk/doc/latex/global/document.tex

@@ -11 +11 @@
 
 %% Document layout
-\documentclass[fontsize = 10pt,
+\documentclass[draft, fontsize = 10pt,
 twoside = semi, abstract = on,
 open = right]{scrreprt}