--- manual/s_examples/baroclinic_gyre/fourlayer.tex 2001/11/13 20:13:54 1.11
+++ manual/s_examples/baroclinic_gyre/fourlayer.tex 2003/08/07 18:27:52 1.15
@@ -1,7 +1,8 @@
-% $Header: /home/ubuntu/mnt/e9_copy/manual/s_examples/baroclinic_gyre/fourlayer.tex,v 1.11 2001/11/13 20:13:54 adcroft Exp $
+% $Header: /home/ubuntu/mnt/e9_copy/manual/s_examples/baroclinic_gyre/fourlayer.tex,v 1.15 2003/08/07 18:27:52 edhill Exp $
% $Name: $
-\section{Example: Four layer Baroclinic Ocean Gyre In Spherical Coordinates}
+\section{Four Layer Baroclinic Ocean Gyre In Spherical Coordinates}
+\label{www:tutorials}
\label{sect:eg-fourlayer}
\bodytext{bgcolor="#FFFFFFFF"}
@@ -26,6 +27,7 @@
for four layers and in a spherical polar coordinate system.
\subsection{Overview}
+\label{www:tutorials}
This example experiment demonstrates using the MITgcm to simulate
a baroclinic, wind-forced, ocean gyre circulation. The experiment
@@ -43,7 +45,7 @@
according to latitude, $\varphi$
\begin{equation}
-\label{EQ:fcori}
+\label{EQ:eg-fourlayer-fcori}
f(\varphi) = 2 \Omega \sin( \varphi )
\end{equation}
@@ -61,7 +63,7 @@
$\tau_0$ is set to $0.1N m^{-2}$.
\\
-Figure \ref{FIG:simulation_config}
+Figure \ref{FIG:eg-fourlayer-simulation_config}
summarizes the configuration simulated.
In contrast to the example in section \ref{sect:eg-baro}, the
current experiment simulates a spherical polar domain. As indicated
@@ -82,14 +84,14 @@
linear
\begin{equation}
-\label{EQ:linear1_eos}
+\label{EQ:eg-fourlayer-linear1_eos}
\rho = \rho_{0} ( 1 - \alpha_{\theta}\theta^{'} )
\end{equation}
\noindent which is implemented in the model as a density anomaly equation
\begin{equation}
-\label{EQ:linear1_eos_pert}
+\label{EQ:eg-fourlayer-linear1_eos_pert}
\rho^{'} = -\rho_{0}\alpha_{\theta}\theta^{'}
\end{equation}
@@ -114,10 +116,11 @@
imposed by setting the potential temperature, $\theta$, in each layer.
The vertical spacing, $\Delta z$, is constant and equal to $500$m.
}
-\label{FIG:simulation_config}
+\label{FIG:eg-fourlayer-simulation_config}
\end{figure}
\subsection{Equations solved}
+\label{www:tutorials}
For this problem
the implicit free surface, {\bf HPE} (see section \ref{sect:hydrostatic_and_quasi-hydrostatic_forms}) form of the
equations described in Marshall et. al \cite{marshall:97a} are
@@ -133,7 +136,7 @@
follows
\begin{eqnarray}
-\label{EQ:model_equations}
+\label{EQ:eg-fourlayer-model_equations}
\frac{Du}{Dt} - fv +
\frac{1}{\rho}\frac{\partial p^{\prime}}{\partial \lambda} -
A_{h}\nabla_{h}^2u - A_{z}\frac{\partial^{2}u}{\partial z^{2}}
@@ -202,6 +205,7 @@
\subsection{Discrete Numerical Configuration}
+\label{www:tutorials}
The domain is discretised with
a uniform grid spacing in latitude and longitude
@@ -261,12 +265,13 @@
\ref{sect:finding_the_pressure_field}.
\subsubsection{Numerical Stability Criteria}
+\label{www:tutorials}
The Laplacian viscosity coefficient, $A_{h}$, is set to $400 m s^{-1}$.
This value is chosen to yield a Munk layer width,
\begin{eqnarray}
-\label{EQ:munk_layer}
+\label{EQ:eg-fourlayer-munk_layer}
M_{w} = \pi ( \frac { A_{h} }{ \beta } )^{\frac{1}{3}}
\end{eqnarray}
@@ -282,7 +287,7 @@
parameter to the horizontal Laplacian friction
\begin{eqnarray}
-\label{EQ:laplacian_stability}
+\label{EQ:eg-fourlayer-laplacian_stability}
S_{l} = 4 \frac{A_{h} \delta t}{{\Delta x}^2}
\end{eqnarray}
@@ -294,7 +299,7 @@
$1\times10^{-2} {\rm m}^2{\rm s}^{-1}$. The associated stability limit
\begin{eqnarray}
-\label{EQ:laplacian_stability_z}
+\label{EQ:eg-fourlayer-laplacian_stability_z}
S_{l} = 4 \frac{A_{z} \delta t}{{\Delta z}^2}
\end{eqnarray}
@@ -307,7 +312,7 @@
\noindent The numerical stability for inertial oscillations
\begin{eqnarray}
-\label{EQ:inertial_stability}
+\label{EQ:eg-fourlayer-inertial_stability}
S_{i} = f^{2} {\delta t}^2
\end{eqnarray}
@@ -320,7 +325,7 @@
speed of $ | \vec{u} | = 2 ms^{-1}$
\begin{eqnarray}
-\label{EQ:cfl_stability}
+\label{EQ:eg-fourlayer-cfl_stability}
C_{a} = \frac{| \vec{u} | \delta t}{ \Delta x}
\end{eqnarray}
@@ -332,7 +337,7 @@
propagating at $2~{\rm m}~{\rm s}^{-1}$
\begin{eqnarray}
-\label{EQ:igw_stability}
+\label{EQ:eg-fourlayer-igw_stability}
S_{c} = \frac{c_{g} \delta t}{ \Delta x}
\end{eqnarray}
@@ -340,6 +345,7 @@
stability limit of 0.25.
\subsection{Code Configuration}
+\label{www:tutorials}
\label{SEC:eg_fourl_code_config}
The model configuration for this experiment resides under the
@@ -354,11 +360,12 @@
\item {\it code/CPP\_OPTIONS.h},
\item {\it code/SIZE.h}.
\end{itemize}
-contain the code customisations and parameter settings for this
-experiments. Below we describe the customisations
-to these files associated with this experiment.
+contain the code customisations and parameter settings for this
+experiment. Below we describe the customisations to these files
+associated with this experiment.
\subsubsection{File {\it input/data}}
+\label{www:tutorials}
This file, reproduced completely below, specifies the main parameters
for the experiment. The parameters that are significant for this configuration
@@ -375,17 +382,19 @@
depth level the initial and reference profiles will be uniform in
$x$ and $y$. The values specified here are read into the
variable
-{\bf
-\begin{rawhtml} \end{rawhtml}
-tRef
-\begin{rawhtml} \end{rawhtml}
-}
+\varlink{tRef}{tRef}
+%{\bf
+%\begin{rawhtml} \end{rawhtml}
+%tRef
+%\begin{rawhtml} \end{rawhtml}
+%}
in the model code, by procedure
-{\it
-\begin{rawhtml} \end{rawhtml}
-INI\_PARMS
-\begin{rawhtml} \end{rawhtml}
-}.
+\filelink{INI\_PARMS}{model-src-ini_parms.F}
+%{\it
+%\begin{rawhtml} \end{rawhtml}
+%INI\_PARMS
+%\begin{rawhtml} \end{rawhtml}
+%}.
%% \codelink{var:tref} tRef \endlink
%% \codelink{file:ini_parms} {\it INI\_PARMS } \endlink
@@ -395,7 +404,7 @@
%% \file{ini_parms}
\newcommand{\VARtref}{
{\bf
-\begin{rawhtml} \end{rawhtml}
+\begin{rawhtml} \end{rawhtml}
tRef
\begin{rawhtml} \end{rawhtml}
}
@@ -409,11 +418,12 @@
({\it ini\_theta.F})
\end{minipage}
}
-{\bf
-\begin{rawhtml} \end{rawhtml}
-goto code
-\begin{rawhtml} \end{rawhtml}
-}
+\filelink{ini\_theta.F}{model-src-ini_theta.F}
+%{\bf
+%\begin{rawhtml} \end{rawhtml}
+%goto code
+%\begin{rawhtml} \end{rawhtml}
+%}
\item Line 6,
@@ -422,36 +432,41 @@
$1 \times 10^{-2} {\rm m^{2}s^{-1}}$. Boundary conditions
for this operator are specified later.
The variable
-{\bf
-\begin{rawhtml} \end{rawhtml}
-viscAz
-\begin{rawhtml} \end{rawhtml}
-}
+\varlink{viscAz}{viscAz}
+%{\bf
+%\begin{rawhtml} \end{rawhtml}
+%viscAz
+%\begin{rawhtml} \end{rawhtml}
+%}
is read in the routine
-{\it
-\begin{rawhtml} \end{rawhtml}
-INI\_PARMS
-\begin{rawhtml} \end{rawhtml}
-}
+\filelink{ini\_parms.F}{model-src-ini_parms.F}
+%{\it
+%\begin{rawhtml} \end{rawhtml}
+%INI\_PARMS
+%\begin{rawhtml} \end{rawhtml}
+%}
and is copied into model general vertical coordinate variable
-{\bf
-\begin{rawhtml} \end{rawhtml}
-viscAr
-\begin{rawhtml} \end{rawhtml}
-}. At each time step, the viscous term contribution to the momentum equations
+\varlink{viscAr}{viscAr}
+%{\bf
+%\begin{rawhtml} \end{rawhtml}
+%viscAr
+%\begin{rawhtml} \end{rawhtml}
+%}.
+At each time step, the viscous term contribution to the momentum equations
is calculated in routine
-{\it S/R CALC\_DIFFUSIVITY}.
+%{\it S/R CALC\_DIFFUSIVITY}.
+\varlink{CALC\_DIFFUSIVITY}{CALC_DIFFUSIVITY}
\fbox{
\begin{minipage}{5.0in}
{\it S/R CALC\_DIFFUSIVITY}({\it calc\_diffusivity.F})
\end{minipage}
}
-{\bf
-\begin{rawhtml} \end{rawhtml}
-goto code
-\begin{rawhtml} \end{rawhtml}
-}
+%{\bf
+%\begin{rawhtml} \end{rawhtml}
+%goto code
+%\begin{rawhtml} \end{rawhtml}
+%}
\item Line 7,
\begin{verbatim}
@@ -461,39 +476,47 @@
$1 \times 10^{-2} {\rm m^{2}s^{-1}}$. Boundary conditions
for this operator are specified later.
The variable
-{\bf
-\begin{rawhtml} \end{rawhtml}
-viscAh
-\begin{rawhtml} \end{rawhtml}
-}
+\varlink{viscAh}{viscAh}
+%{\bf
+%\begin{rawhtml} \end{rawhtml}
+%viscAh
+%\begin{rawhtml} \end{rawhtml}
+%}
is read in the routine
-{\it
-\begin{rawhtml} \end{rawhtml}
-INI\_PARMS
-\begin{rawhtml} \end{rawhtml}
-} and applied in routines {\it CALC\_MOM\_RHS} and {\it CALC\_GW}.
+\varlink{INI\_PARMS}{INI_PARMS}
+%{\it
+%\begin{rawhtml} \end{rawhtml}
+%INI\_PARMS
+%\begin{rawhtml} \end{rawhtml}
+%}
+and applied in routines
+%{\it CALC\_MOM\_RHS} and {\it CALC\_GW}.
+\varlink{CALC\_MOM\_RHS}{CALC_MOM_RHS}
+and
+\varlink{CALC\_GW}{CALC_GW}.
+
\fbox{
\begin{minipage}{5.0in}
{\it S/R CALC\_MOM\_RHS}({\it calc\_mom\_rhs.F})
\end{minipage}
}
-{\bf
-\begin{rawhtml} \end{rawhtml}
-goto code
-\begin{rawhtml} \end{rawhtml}
-}
+%{\bf
+%\begin{rawhtml} \end{rawhtml}
+%goto code
+%\begin{rawhtml} \end{rawhtml}
+%}
\fbox{
\begin{minipage}{5.0in}
{\it S/R CALC\_GW}({\it calc\_gw.F})
\end{minipage}
}
-{\bf
-\begin{rawhtml} \end{rawhtml}
-goto code
-\begin{rawhtml} \end{rawhtml}
-}
+%{\bf
+%\begin{rawhtml} \end{rawhtml}
+%goto code
+%\begin{rawhtml} \end{rawhtml}
+%}
\item Lines 8,
\begin{verbatim}
@@ -504,18 +527,21 @@
e.g. $\frac{\partial u}{\partial y}$=0 along boundaries in $y$ and
$\frac{\partial v}{\partial x}$=0 along boundaries in $x$.
The variable
-{\bf
-\begin{rawhtml} \end{rawhtml}
-no\_slip\_sides
-\begin{rawhtml} \end{rawhtml}
-}
+\varlink{no\_slip\_sides}{no_slip_sides}
+%{\bf
+%\begin{rawhtml} \end{rawhtml}
+%no\_slip\_sides
+%\begin{rawhtml} \end{rawhtml}
+%}
is read in the routine
-{\it
-\begin{rawhtml} \end{rawhtml}
-INI\_PARMS
-\begin{rawhtml} \end{rawhtml}
-} and the boundary condition is evaluated in routine
-{\it S/R CALC\_MOM\_RHS}.
+\varlink{INI\_PARMS}{INI_PARMS}
+%{\it
+%\begin{rawhtml} \end{rawhtml}
+%INI\_PARMS
+%\begin{rawhtml} \end{rawhtml}
+%}
+and the boundary condition is evaluated in routine
+%{\it S/R CALC\_MOM\_RHS}.
\fbox{
@@ -524,7 +550,7 @@
\end{minipage}
}
{\bf
-\begin{rawhtml} \end{rawhtml}
+\begin{rawhtml} \end{rawhtml}
goto code
\begin{rawhtml} \end{rawhtml}
}
@@ -538,13 +564,13 @@
e.g. $u=v=0$ at $z=-H$, where $H$ is the local depth of the domain.
The variable
{\bf
-\begin{rawhtml} \end{rawhtml}
+\begin{rawhtml} \end{rawhtml}
no\_slip\_bottom
\begin{rawhtml} \end{rawhtml}
}
is read in the routine
{\it
-\begin{rawhtml} \end{rawhtml}
+\begin{rawhtml} \end{rawhtml}
INI\_PARMS
\begin{rawhtml} \end{rawhtml}
} and is applied in the routine {\it S/R CALC\_MOM\_RHS}.
@@ -555,7 +581,7 @@
\end{minipage}
}
{\bf
-\begin{rawhtml} \end{rawhtml}
+\begin{rawhtml} \end{rawhtml}
goto code
\begin{rawhtml} \end{rawhtml}
}
@@ -570,13 +596,13 @@
all boundaries.
The variable
{\bf
-\begin{rawhtml} \end{rawhtml}
+\begin{rawhtml} \end{rawhtml}
diffKhT
\begin{rawhtml} \end{rawhtml}
}
is read in the routine
{\it
-\begin{rawhtml} \end{rawhtml}
+\begin{rawhtml} \end{rawhtml}
INI\_PARMS
\begin{rawhtml} \end{rawhtml}
} and used in routine {\it S/R CALC\_GT}.
@@ -586,7 +612,7 @@
\end{minipage}
}
{\bf
-\begin{rawhtml} \end{rawhtml}
+\begin{rawhtml} \end{rawhtml}
goto code
\begin{rawhtml} \end{rawhtml}
}
@@ -600,19 +626,19 @@
operator is $\frac{\partial}{\partial z}$ = 0 on all boundaries.
The variable
{\bf
-\begin{rawhtml} \end{rawhtml}
+\begin{rawhtml} \end{rawhtml}
diffKzT
\begin{rawhtml} \end{rawhtml}
}
is read in the routine
{\it
-\begin{rawhtml} \end{rawhtml}
+\begin{rawhtml} \end{rawhtml}
INI\_PARMS
\begin{rawhtml} \end{rawhtml}
}.
It is copied into model general vertical coordinate variable
{\bf
-\begin{rawhtml} \end{rawhtml}
+\begin{rawhtml} \end{rawhtml}
diffKrT
\begin{rawhtml} \end{rawhtml}
} which is used in routine {\it S/R CALC\_DIFFUSIVITY}.
@@ -622,7 +648,7 @@
\end{minipage}
}
{\bf
-\begin{rawhtml} \end{rawhtml}
+\begin{rawhtml} \end{rawhtml}
goto code
\begin{rawhtml} \end{rawhtml}
}
@@ -637,13 +663,13 @@
to $2 \times 10^{-4}\,{\rm degrees}^{-1}$
The variable
{\bf
-\begin{rawhtml} \end{rawhtml}
+\begin{rawhtml} \end{rawhtml}
tAlpha
\begin{rawhtml} \end{rawhtml}
}
is read in the routine
{\it
-\begin{rawhtml} \end{rawhtml}
+\begin{rawhtml} \end{rawhtml}
INI\_PARMS
\begin{rawhtml} \end{rawhtml}
}. The routine {\it S/R FIND\_RHO} makes use of {\bf tAlpha}.
@@ -654,7 +680,7 @@
\end{minipage}
}
{\bf
-\begin{rawhtml} \end{rawhtml}
+\begin{rawhtml} \end{rawhtml}
goto code
\begin{rawhtml} \end{rawhtml}
}
@@ -666,13 +692,13 @@
This line selects the linear form of the equation of state.
The variable
{\bf
-\begin{rawhtml} \end{rawhtml}
+\begin{rawhtml} \end{rawhtml}
eosType
\begin{rawhtml} \end{rawhtml}
}
is read in the routine
{\it
-\begin{rawhtml} \end{rawhtml}
+\begin{rawhtml} \end{rawhtml}
INI\_PARMS
\begin{rawhtml} \end{rawhtml}
}. The values of {\bf eosType} sets which formula in routine
@@ -684,7 +710,7 @@
\end{minipage}
}
{\bf
-\begin{rawhtml} \end{rawhtml}
+\begin{rawhtml} \end{rawhtml}
goto code
\begin{rawhtml} \end{rawhtml}
}
@@ -702,13 +728,13 @@
on spherical polar geometry.
The variable
{\bf
-\begin{rawhtml} \end{rawhtml}
+\begin{rawhtml} \end{rawhtml}
usingSphericalPolarGrid
\begin{rawhtml} \end{rawhtml}
}
is read in the routine
{\it
-\begin{rawhtml} \end{rawhtml}
+\begin{rawhtml} \end{rawhtml}
INI\_PARMS
\begin{rawhtml} \end{rawhtml}
}. When set to {\bf .TRUE.} the settings of {\bf delX} and {\bf delY} are
@@ -721,7 +747,7 @@
\end{minipage}
}
{\bf
-\begin{rawhtml} \end{rawhtml}
+\begin{rawhtml} \end{rawhtml}
goto code
\begin{rawhtml} \end{rawhtml}
}
@@ -739,13 +765,13 @@
not alter the kernel equation discretisation.
The variable
{\bf
-\begin{rawhtml} \end{rawhtml}
+\begin{rawhtml} \end{rawhtml}
phiMin
\begin{rawhtml} \end{rawhtml}
}
is read in the routine
{\it
-\begin{rawhtml} \end{rawhtml}
+\begin{rawhtml} \end{rawhtml}
INI\_PARMS
\begin{rawhtml} \end{rawhtml}
} and is used in routine {\it INI\_SPEHRICAL\_POLAR\_GRID}.
@@ -756,7 +782,7 @@
\end{minipage}
}
{\bf
-\begin{rawhtml} \end{rawhtml}
+\begin{rawhtml} \end{rawhtml}
goto code
\begin{rawhtml} \end{rawhtml}
}
@@ -769,13 +795,13 @@
in the discrete grid to $1^{\circ}$ in longitude.
The variable
{\bf
-\begin{rawhtml} \end{rawhtml}
+\begin{rawhtml} \end{rawhtml}
delX
\begin{rawhtml} \end{rawhtml}
}
is read in the routine
{\it
-\begin{rawhtml} \end{rawhtml}
+\begin{rawhtml} \end{rawhtml}
INI\_PARMS
\begin{rawhtml} \end{rawhtml}
} and is used in routine {\it INI\_SPEHRICAL\_POLAR\_GRID}.
@@ -786,7 +812,7 @@
\end{minipage}
}
{\bf
-\begin{rawhtml} \end{rawhtml}
+\begin{rawhtml} \end{rawhtml}
goto code
\begin{rawhtml} \end{rawhtml}
}
@@ -799,13 +825,13 @@
in the discrete grid to $1^{\circ}$ in latitude.
The variable
{\bf
-\begin{rawhtml} \end{rawhtml}
+\begin{rawhtml} \end{rawhtml}
delY
\begin{rawhtml} \end{rawhtml}
}
is read in the routine
{\it
-\begin{rawhtml} \end{rawhtml}
+\begin{rawhtml} \end{rawhtml}
INI\_PARMS
\begin{rawhtml} \end{rawhtml}
} and is used in routine {\it INI\_SPEHRICAL\_POLAR\_GRID}.
@@ -816,7 +842,7 @@
\end{minipage}
}
{\bf
-\begin{rawhtml} \end{rawhtml}
+\begin{rawhtml} \end{rawhtml}
goto code
\begin{rawhtml} \end{rawhtml}
}
@@ -830,20 +856,20 @@
is $2\,{\rm km}$.
The variable
{\bf
-\begin{rawhtml} \end{rawhtml}
+\begin{rawhtml} \end{rawhtml}
delZ
\begin{rawhtml} \end{rawhtml}
}
is read in the routine
{\it
-\begin{rawhtml} \end{rawhtml}
+\begin{rawhtml} \end{rawhtml}
INI\_PARMS
\begin{rawhtml} \end{rawhtml}
}.
It is copied into the internal
model coordinate variable
{\bf
-\begin{rawhtml} \end{rawhtml}
+\begin{rawhtml} \end{rawhtml}
delR
\begin{rawhtml} \end{rawhtml}
} which is used in routine {\it INI\_VERTICAL\_GRID}.
@@ -854,7 +880,7 @@
\end{minipage}
}
{\bf
-\begin{rawhtml} \end{rawhtml}
+\begin{rawhtml} \end{rawhtml}
goto code
\begin{rawhtml} \end{rawhtml}
}
@@ -876,13 +902,13 @@
bathymetry file.
The variable
{\bf
-\begin{rawhtml} \end{rawhtml}
+\begin{rawhtml} \end{rawhtml}
bathyFile
\begin{rawhtml} \end{rawhtml}
}
is read in the routine
{\it
-\begin{rawhtml} \end{rawhtml}
+\begin{rawhtml} \end{rawhtml}
INI\_PARMS
\begin{rawhtml} \end{rawhtml}
}. The bathymetry file is read in the routine {\it INI\_DEPTHS}.
@@ -893,7 +919,7 @@
\end{minipage}
}
{\bf
-\begin{rawhtml} \end{rawhtml}
+\begin{rawhtml} \end{rawhtml}
goto code
\begin{rawhtml} \end{rawhtml}
}
@@ -912,13 +938,13 @@
file.
The variable
{\bf
-\begin{rawhtml} \end{rawhtml}
+\begin{rawhtml} \end{rawhtml}
zonalWindFile
\begin{rawhtml} \end{rawhtml}
}
is read in the routine
{\it
-\begin{rawhtml} \end{rawhtml}
+\begin{rawhtml} \end{rawhtml}
INI\_PARMS
\begin{rawhtml} \end{rawhtml}
}. The wind-stress file is read in the routine
@@ -930,7 +956,7 @@
\end{minipage}
}
{\bf
-\begin{rawhtml} \end{rawhtml}
+\begin{rawhtml} \end{rawhtml}
goto code
\begin{rawhtml} \end{rawhtml}
}
@@ -946,16 +972,19 @@
\begin{rawhtml}\end{rawhtml}
\subsubsection{File {\it input/data.pkg}}
+\label{www:tutorials}
This file uses standard default values and does not contain
customisations for this experiment.
\subsubsection{File {\it input/eedata}}
+\label{www:tutorials}
This file uses standard default values and does not contain
customisations for this experiment.
\subsubsection{File {\it input/windx.sin\_y}}
+\label{www:tutorials}
The {\it input/windx.sin\_y} file specifies a two-dimensional ($x,y$)
map of wind stress ,$\tau_{x}$, values. The units used are $Nm^{-2}$ (the
@@ -969,6 +998,7 @@
code for creating the {\it input/windx.sin\_y} file.
\subsubsection{File {\it input/topog.box}}
+\label{www:tutorials}
The {\it input/topog.box} file specifies a two-dimensional ($x,y$)
@@ -980,6 +1010,7 @@
code for creating the {\it input/topog.box} file.
\subsubsection{File {\it code/SIZE.h}}
+\label{www:tutorials}
Two lines are customized in this file for the current experiment
@@ -1006,17 +1037,20 @@
\end{small}
\subsubsection{File {\it code/CPP\_OPTIONS.h}}
+\label{www:tutorials}
This file uses standard default values and does not contain
customisations for this experiment.
\subsubsection{File {\it code/CPP\_EEOPTIONS.h}}
+\label{www:tutorials}
This file uses standard default values and does not contain
customisations for this experiment.
\subsubsection{Other Files }
+\label{www:tutorials}
Other files relevant to this experiment are
\begin{itemize}
@@ -1029,15 +1063,18 @@
\end{itemize}
\subsection{Running The Example}
+\label{www:tutorials}
\label{SEC:running_the_example}
\subsubsection{Code Download}
+\label{www:tutorials}
In order to run the examples you must first download the code distribution.
Instructions for downloading the code can be found in section
\ref{sect:obtainingCode}.
\subsubsection{Experiment Location}
+\label{www:tutorials}
This example experiments is located under the release sub-directory
@@ -1045,6 +1082,7 @@
{\it verification/exp2/ }
\subsubsection{Running the Experiment}
+\label{www:tutorials}
To run the experiment