Changeset 4147 for branches/2013/dev_LOCEAN_2013/DOC/TexFiles/Chapters/Chap_TRA.tex

Timestamp:

2013-11-04T12:51:55+01:00 (10 years ago)

Author:

cetlod

Message:

merge in dev_LOCEAN_2013, the 1st development branch dev_r3853_CNRS9_Confsetting, from its starting point ( r3853 ) on the trunk: see ticket #1169

File:

• branches/2013/dev_LOCEAN_2013/DOC/TexFiles/Chapters/Chap_TRA.tex (modified) (11 diffs)

branches/2013/dev_LOCEAN_2013/DOC/TexFiles/Chapters/Chap_TRA.tex

@@ -1 +1 @@
 % ================================================================
-% Chapter 1 Ñ Ocean Tracers (TRA)
+% Chapter 1 � Ocean Tracers (TRA)
 % ================================================================
 \chapter{Ocean Tracers (TRA)}
@@ -137 +137 @@
 \textit{effective} velocity ($i.e.$ the sum of the eulerian and eiv velocities) which is used.
 
-The choice of an advection scheme is made in the \textit{nam\_traadv} namelist, by 
+The choice of an advection scheme is made in the \textit{\ngn{nam\_traadv}} namelist, by 
 setting to \textit{true} one and only one of the logicals \textit{ln\_traadv\_xxx}. The 
 corresponding code can be found in the \textit{traadv\_xxx.F90} module, where 
@@ -441 +441 @@
 %-------------------------------------------------------------------------------------------------------------
  
+Options are defined through the  \ngn{namtra\_ldf} namelist variables.
 The options available for lateral diffusion are a laplacian (rotated or not) 
 or a biharmonic operator, the latter being more scale-selective (more 
@@ -602 +603 @@
 %--------------------------------------------------------------------------------------------------------------
 
+Options are defined through the  \ngn{namzdf} namelist variables.
 The formulation of the vertical subgrid scale tracer physics is the same 
 for all the vertical coordinates, and is based on a laplacian operator. 
@@ -757 +759 @@
 %--------------------------------------------------------------------------------------------------------------
 
+Options are defined through the  \ngn{namtra\_qsr} namelist variables.
 When the penetrative solar radiation option is used (\np{ln\_flxqsr}=true), 
 the solar radiation penetrates the top few tens of meters of the ocean. If it is not used 
@@ -879 +882 @@
 Bottom Water) by a few Sverdrups  \citep{Emile-Geay_Madec_OS09}. 
 
+Options are defined through the  \ngn{namtra\_bbc} namelist variables.
 The presence of geothermal heating is controlled by setting the namelist 
 parameter  \np{ln\_trabbc} to true. Then, when \np{nn\_geoflx} is set to 1, 
@@ -897 +901 @@
 %--------------------------------------------------------------------------------------------------------------
 
+Options are defined through the  \ngn{nambbl} namelist variables.
 In a $z$-coordinate configuration, the bottom topography is represented by a 
 series of discrete steps. This is not adequate to represent gravity driven 
@@ -1066 +1071 @@
 where $\gamma$ is the inverse of a time scale, and $T_o$ and $S_o$ 
 are given temperature and salinity fields (usually a climatology). 
+Options are defined through the  \ngn{namtra\_dmp} namelist variables.
 The restoring term is added when the namelist parameter \np{ln\_tradmp} is set to true. 
 It also requires that both \np{ln\_tsd\_init} and \np{ln\_tsd\_tradmp} are set to true
@@ -1128 +1134 @@
 %--------------------------------------------------------------------------------------------------------------
 
+Options are defined through the  \ngn{namdom} namelist variables.
 The general framework for tracer time stepping is a modified leap-frog scheme 
 \citep{Leclair_Madec_OM09}, $i.e.$ a three level centred time scheme associated 
@@ -1205 +1212 @@
 \citep{Gill1982}.
 
+Options are defined through the  \ngn{nameos} namelist variables.
 The default option (namelist parameter \np{nn\_eos}=0) is the \citet{JackMcD1995} 
 equation of state. Its use is highly recommended. However, for process studies, 
@@ -1222 +1230 @@
 coefficients, and $\rho_o$, the reference volumic mass, $rau0$. 
 ($\alpha$ and $\beta$ can be modified through the \np{rn\_alpha} and 
-\np{rn\_beta} namelist parameters). Note that when $d_a$ is a function 
+\np{rn\_beta} namelist variables). Note that when $d_a$ is a function 
 of $T$ only (\np{nn\_eos}=1), the salinity is a passive tracer and can be 
 used as such.