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\bodytext{bgcolor="#FFFFFFFF"} |
\bodytext{bgcolor="#FFFFFFFF"} |
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%\begin{center} |
%\begin{center} |
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%{\Large \bf Using MITgcm to Simulate a Rotating Tank in Cylindrical |
%{\Large \bf Using MITgcm to Simulate a Rotating Tank in Cylindrical |
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%Coordinates} |
%Coordinates} |
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% |
% |
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%\vspace*{4mm} |
%\vspace*{4mm} |
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% |
% |
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%\vspace*{3mm} |
%\vspace*{3mm} |
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%{\large June 2004} |
%{\large May 2001} |
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%\end{center} |
%\end{center} |
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This is the first in a series of tutorials describing |
\section{A Rotating Tank in Cylindrical Coordinates} |
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example MITgcm numerical experiments. The example experiments |
\label{sect:eg-tank} |
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include both straightforward examples of idealized geophysical |
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fluid simulations and more involved cases encompassing |
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large scale modeling and |
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automatic differentiation. Both hydrostatic and non-hydrostatic |
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experiments are presented, as well as experiments employing |
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Cartesian, spherical-polar and cube-sphere coordinate systems. |
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These ``case study'' documents include information describing |
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the experimental configuration and detailed information on how to |
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configure the MITgcm code and input files for each experiment. |
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\section{Barotropic Ocean Gyre In Cartesian Coordinates} |
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\label{sect:eg-baro} |
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\label{www:tutorials} |
\label{www:tutorials} |
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\begin{rawhtml} |
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<!-- CMIREDIR:eg-tank: --> |
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\end{rawhtml} |
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\begin{center} |
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(in directory: {\it verification/rotating\_tank/}) |
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\end{center} |
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\subsection{Overview} |
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\label{www:tutorials} |
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This example configuration demonstrates using the MITgcm to simulate a |
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laboratory demonstration using a differentially heated rotating |
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annulus of water. The simulation is configured for a laboratory scale |
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on a $3^{\circ}\times1\mathrm{cm}$ cyclindrical grid with twenty-nine |
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vertical levels of 0.5cm each. This is a typical laboratory setup for |
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illustration principles of GFD, as well as for a laboratory data |
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assimilation project. The files for this experiment can be found in |
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the verification directory under rotating\_tank. |
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\\ |
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example illustration from GFD lab here |
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\\ |
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\subsection{Equations Solved} |
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\label{www:tutorials} |
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The model is configured in hydrostatic form. The implicit free surface form of the |
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\subsection{Discrete Numerical Configuration} |
\subsection{Equations Solved} |
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\label{www:tutorials} |
\label{www:tutorials} |
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The domain is discretised with |
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a uniform grid spacing in the horizontal set to |
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$\Delta x=\Delta y=20$~km, so |
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that there are sixty grid cells in the $x$ and $y$ directions. Vertically the |
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model is configured with a single layer with depth, $\Delta z$, of $5000$~m. |
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\subsubsection{Numerical Stability Criteria} |
\subsection{Discrete Numerical Configuration} |
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\label{www:tutorials} |
\label{www:tutorials} |
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The domain is discretised with a uniform cylindrical grid spacing in |
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the horizontal set to $\Delta a=1$~cm and $\Delta \phi=3^{\circ}$, so |
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that there are 120 grid cells in the azimuthal direction and |
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thirty-one grid cells in the radial, representing a tank 62cm in |
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diameter. The bathymetry file sets the depth=0 in the nine lowest |
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radial rows to represent the central of the annulus. Vertically the |
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model is configured with twenty-nine layers of uniform 0.5cm |
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thickness. |
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\\ |
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something about heat flux |
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\subsection{Code Configuration} |
\subsection{Code Configuration} |
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\label{www:tutorials} |
\label{www:tutorials} |
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\label{SEC:eg-baro-code_config} |
\label{SEC:eg-baro-code_config} |
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The model configuration for this experiment resides under the |
The model configuration for this experiment resides under the |
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directory {\it verification/exp0/}. The experiment files |
directory {\it verification/rotatingi\_tank/}. The experiment files |
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\begin{itemize} |
\begin{itemize} |
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\item {\it input/data} |
\item {\it input/data} |
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\item {\it input/data.pkg} |
\item {\it input/data.pkg} |
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\item {\it input/eedata}, |
\item {\it input/eedata}, |
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\item {\it input/windx.sin\_y}, |
\item {\it input/bathyPol.bin}, |
75 |
\item {\it input/topog.box}, |
\item {\it input/thetaPol.bin}, |
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\item {\it code/CPP\_EEOPTIONS.h} |
\item {\it code/CPP\_EEOPTIONS.h} |
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\item {\it code/CPP\_OPTIONS.h}, |
\item {\it code/CPP\_OPTIONS.h}, |
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\item {\it code/SIZE.h}. |
\item {\it code/SIZE.h}. |
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\end{itemize} |
\end{itemize} |
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|
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contain the code customizations and parameter settings for this |
contain the code customizations and parameter settings for this |
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experiments. Below we describe the customizations |
experiments. Below we describe the customizations |
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to these files associated with this experiment. |
to these files associated with this experiment. |
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\begin{itemize} |
\begin{itemize} |
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\item Line 7, \begin{verbatim} viscAh=4.E2, \end{verbatim} this line sets |
\item Lines 9-10, \begin{verbatim} |
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the Laplacian friction coefficient to $400 m^2s^{-1}$ |
viscAh=5.0E-6, |
96 |
\item Line 10, \begin{verbatim} beta=1.E-11, \end{verbatim} this line sets |
viscAz=5.0E-6, |
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$\beta$ (the gradient of the coriolis parameter, $f$) to $10^{-11} s^{-1}m^{-1}$ |
\end{verbatim} |
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These lines set the Laplacian friction coefficient in the horizontal |
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and vertical, respectively. Note that they are several orders of |
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magnitude smaller than the other examples due to the small scale of |
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this example. |
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\item Lines 13-16, \begin{verbatim} |
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diffKhT=2.5E-6, |
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diffKzT=2.5E-6, |
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diffKhS=1.0E-6, |
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diffKzS=1.0E-6, |
110 |
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\end{verbatim} |
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These lines set horizontal and vertical diffusion coefficients for |
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temperature and salinity. Similarly to the friction coefficients, the |
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values are a couple of orders of magnitude less than most |
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configurations. |
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\item Lines 15 and 16 |
\item Line 17, \begin{verbatim}f0=0.5 , \end{verbatim} this line sets the |
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coriolis term, and represents a tank spinning at about 2.4 rpm. |
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|
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\item Lines 23 and 24 |
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\begin{verbatim} |
\begin{verbatim} |
125 |
rigidLid=.FALSE., |
rigidLid=.TRUE., |
126 |
implicitFreeSurface=.TRUE., |
implicitFreeSurface=.FALSE., |
127 |
\end{verbatim} |
\end{verbatim} |
128 |
these lines suppress the rigid lid formulation of the surface |
|
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pressure inverter and activate the implicit free surface form |
These lines activate the rigid lid formulation of the surface |
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pressure inverter and suppress the implicit free surface form |
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of the pressure inverter. |
of the pressure inverter. |
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\item Line 27, |
\item Line 40, |
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\begin{verbatim} |
\begin{verbatim} |
135 |
startTime=0, |
nIter=0, |
136 |
\end{verbatim} |
\end{verbatim} |
137 |
this line indicates that the experiment should start from $t=0$ |
This line indicates that the experiment should start from $t=0$ and |
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and implicitly suppresses searching for checkpoint files associated |
implicitly suppresses searching for checkpoint files associated with |
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with restarting an numerical integration from a previously saved state. |
restarting an numerical integration from a previously saved state. |
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Instead, the file thetaPol.bin will be loaded to initialized the |
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temperature fields as indicated below, and other variables will be |
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initialized to their defaults. |
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\item Line 29, |
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\begin{verbatim} |
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endTime=12000, |
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\end{verbatim} |
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this line indicates that the experiment should start finish at $t=12000s$. |
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A restart file will be written at this time that will enable the |
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simulation to be continued from this point. |
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\item Line 30, |
\item Line 43, |
146 |
\begin{verbatim} |
\begin{verbatim} |
147 |
deltaTmom=1200, |
deltaT=0.1, |
148 |
\end{verbatim} |
\end{verbatim} |
149 |
This line sets the momentum equation timestep to $1200s$. |
This line sets the integration timestep to $0.1s$. This is an |
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unsually small value among the examples due to the small physical |
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scale of the experiment. Using the ensemble Kalman filter to produce |
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input fields can necessitate even shorter timesteps. |
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\item Line 39, |
\item Line 56, |
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\begin{verbatim} |
\begin{verbatim} |
156 |
usingCartesianGrid=.TRUE., |
usingCylindricalGrid=.TRUE., |
157 |
\end{verbatim} |
\end{verbatim} |
158 |
This line requests that the simulation be performed in a |
This line requests that the simulation be performed in a |
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Cartesian coordinate system. |
cylindrical coordinate system. |
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\item Line 41, |
\item Line 57, |
162 |
\begin{verbatim} |
\begin{verbatim} |
163 |
delX=60*20E3, |
dXspacing=3, |
164 |
\end{verbatim} |
\end{verbatim} |
165 |
This line sets the horizontal grid spacing between each x-coordinate line |
This line sets the azimuthal grid spacing between each $x$-coordinate line |
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in the discrete grid. The syntax indicates that the discrete grid |
in the discrete grid. The syntax indicates that the discrete grid |
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should be comprise of $60$ grid lines each separated by $20 \times 10^{3}m$ |
should be comprised of $120$ grid lines each separated by $3^{\circ}$. |
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($20$~km). |
|
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\item Line 42, |
\item Line 58, |
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\begin{verbatim} |
\begin{verbatim} |
172 |
delY=60*20E3, |
dYspacing=0.01, |
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\end{verbatim} |
\end{verbatim} |
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This line sets the horizontal grid spacing between each y-coordinate line |
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in the discrete grid to $20 \times 10^{3}m$ ($20$~km). |
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\item Line 43, |
This line sets the radial cylindrical grid spacing between each |
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$a$-coordinate line in the discrete grid to $1cm$. |
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\item Line 59, |
179 |
\begin{verbatim} |
\begin{verbatim} |
180 |
delZ=5000, |
delZ=29*0.005, |
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\end{verbatim} |
\end{verbatim} |
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This line sets the vertical grid spacing between each z-coordinate line |
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in the discrete grid to $5000m$ ($5$~km). |
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\item Line 46, |
This line sets the vertical grid spacing between each of 29 |
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z-coordinate lines in the discrete grid to $0.005m$ ($5$~mm). |
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\item Line 64, |
187 |
\begin{verbatim} |
\begin{verbatim} |
188 |
bathyFile='topog.box' |
bathyFile='bathyPol.bin', |
189 |
\end{verbatim} |
\end{verbatim} |
190 |
This line specifies the name of the file from which the domain |
This line specifies the name of the file from which the domain |
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bathymetry is read. This file is a two-dimensional ($x,y$) map of |
``bathymetry'' (tank depth) is read. This file is a two-dimensional |
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($a,\phi$) map of |
193 |
depths. This file is assumed to contain 64-bit binary numbers |
depths. This file is assumed to contain 64-bit binary numbers |
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giving the depth of the model at each grid cell, ordered with the x |
giving the depth of the model at each grid cell, ordered with the $\phi$ |
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coordinate varying fastest. The points are ordered from low coordinate |
coordinate varying fastest. The points are ordered from low coordinate |
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to high coordinate for both axes. The units and orientation of the |
to high coordinate for both axes. The units and orientation of the |
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depths in this file are the same as used in the MITgcm code. In this |
depths in this file are the same as used in the MITgcm code. In this |
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experiment, a depth of $0m$ indicates a solid wall and a depth |
experiment, a depth of $0m$ indicates an area outside of the tank |
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of $-5000m$ indicates open ocean. The matlab program |
and a depth |
200 |
{\it input/gendata.m} shows an example of how to generate a |
f $-0.145m$ indicates the tank itself. |
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bathymetry file. |
|
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\item Line 65, |
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\begin{verbatim} |
204 |
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hydrogThetaFile='thetaPol.bin', |
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\end{verbatim} |
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This line specifies the name of the file from which the initial values |
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of temperature |
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are read. This file is a three-dimensional |
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($x,y,z$) map and is enumerated and formatted in the same manner as the |
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bathymetry file. |
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\item Line 49, |
\item Lines 66 and 67 |
213 |
\begin{verbatim} |
\begin{verbatim} |
214 |
zonalWindFile='windx.sin_y' |
tCylIn = 0 |
215 |
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tCylOut = 20 |
216 |
\end{verbatim} |
\end{verbatim} |
217 |
This line specifies the name of the file from which the x-direction |
These line specify the temperatures in degrees Celsius of the interior |
218 |
surface wind stress is read. This file is also a two-dimensional |
and exterior walls of the tank -- typically taken to be icewater on |
219 |
($x,y$) map and is enumerated and formatted in the same manner as the |
the inside and room temperature on the outside. |
220 |
bathymetry file. The matlab program {\it input/gendata.m} includes example |
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code to generate a valid {\bf zonalWindFile} file. |
|
221 |
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|
222 |
\end{itemize} |
\end{itemize} |
223 |
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\noindent other lines in the file {\it input/data} are standard values |
\noindent Other lines in the file {\it input/data} are standard values |
225 |
that are described in the MITgcm Getting Started and MITgcm Parameters |
that are described in the MITgcm Getting Started and MITgcm Parameters |
226 |
notes. |
notes. |
227 |
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|
228 |
%%\begin{small} |
\begin{small} |
229 |
%%\input{part3/case_studies/barotropic_gyre/input/data} |
\input{part3/case_studies/rotating_tank/input/data} |
230 |
%%\end{small} |
\end{small} |
231 |
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|
232 |
\subsubsection{File {\it input/data.pkg}} |
\subsubsection{File {\it input/data.pkg}} |
233 |
\label{www:tutorials} |
\label{www:tutorials} |
241 |
This file uses standard default values and does not contain |
This file uses standard default values and does not contain |
242 |
customizations for this experiment. |
customizations for this experiment. |
243 |
|
|
244 |
\subsubsection{File {\it input/windx.sin\_y}} |
\subsubsection{File {\it input/thetaPol.bin}} |
245 |
\label{www:tutorials} |
\label{www:tutorials} |
246 |
|
|
247 |
The {\it input/windx.sin\_y} file specifies a two-dimensional ($x,y$) |
The {\it input/thetaPol.bin} file specifies a three-dimensional ($x,y,z$) |
248 |
map of wind stress ,$\tau_{x}$, values. The units used are $Nm^{-2}$. |
map of initial values of $\theta$ in degrees Celsius. This particular |
249 |
Although $\tau_{x}$ is only a function of $y$n in this experiment |
experiment is set to random values x around 20C to provide initial |
250 |
this file must still define a complete two-dimensional map in order |
perturbations. |
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to be compatible with the standard code for loading forcing fields |
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in MITgcm. The included matlab program {\it input/gendata.m} gives a complete |
|
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code for creating the {\it input/windx.sin\_y} file. |
|
251 |
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|
252 |
\subsubsection{File {\it input/topog.box}} |
\subsubsection{File {\it input/bathyPol.bin}} |
253 |
\label{www:tutorials} |
\label{www:tutorials} |
254 |
|
|
255 |
|
|
256 |
The {\it input/topog.box} file specifies a two-dimensional ($x,y$) |
The {\it input/bathyPol.bin} file specifies a two-dimensional ($x,y$) |
257 |
map of depth values. For this experiment values are either |
map of depth values. For this experiment values are either |
258 |
$0m$ or {\bf -delZ}m, corresponding respectively to a wall or to deep |
$0m$ or {\bf -delZ}m, corresponding respectively to outside or inside of |
259 |
ocean. The file contains a raw binary stream of data that is enumerated |
the tank. The file contains a raw binary stream of data that is enumerated |
260 |
in the same way as standard MITgcm two-dimensional, horizontal arrays. |
in the same way as standard MITgcm two-dimensional, horizontal arrays. |
|
The included matlab program {\it input/gendata.m} gives a complete |
|
|
code for creating the {\it input/topog.box} file. |
|
261 |
|
|
262 |
\subsubsection{File {\it code/SIZE.h}} |
\subsubsection{File {\it code/SIZE.h}} |
263 |
\label{www:tutorials} |
\label{www:tutorials} |
267 |
\begin{itemize} |
\begin{itemize} |
268 |
|
|
269 |
\item Line 39, |
\item Line 39, |
270 |
\begin{verbatim} sNx=60, \end{verbatim} this line sets |
\begin{verbatim} sNx=120, \end{verbatim} this line sets |
271 |
the lateral domain extent in grid points for the |
the lateral domain extent in grid points for the |
272 |
axis aligned with the x-coordinate. |
axis aligned with the x-coordinate. |
273 |
|
|
274 |
\item Line 40, |
\item Line 40, |
275 |
\begin{verbatim} sNy=60, \end{verbatim} this line sets |
\begin{verbatim} sNy=31, \end{verbatim} this line sets |
276 |
the lateral domain extent in grid points for the |
the lateral domain extent in grid points for the |
277 |
axis aligned with the y-coordinate. |
axis aligned with the y-coordinate. |
278 |
|
|
279 |
\end{itemize} |
\end{itemize} |
280 |
|
|
281 |
\begin{small} |
\begin{small} |
282 |
\input{part3/case_studies/barotropic_gyre/code/SIZE.h} |
\input{part3/case_studies/rotating_tank/code/SIZE.h} |
283 |
\end{small} |
\end{small} |
284 |
|
|
285 |
\subsubsection{File {\it code/CPP\_OPTIONS.h}} |
\subsubsection{File {\it code/CPP\_OPTIONS.h}} |