s_examples/advection_in_gyre/adv_gyre.tex

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\section[Gyre Advection Example]{Ocean Gyre Advection Schemes}
\label{www:tutorials}
\label{sect:eg-adv-gyre}
\begin{rawhtml}
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\end{rawhtml}

Author: Oliver Jahn and Chris Hill


This set of examples is based on the barotropic and baroclinic gyre MITgcm configurations,
that are described in the tutorial sections \ref{sect:eg-baro} and \ref{sect:eg-fourlayer}. 
The examples in this section explain how to introduce a passive tracer into the flow 
field of the barotropic and baroclinic gyre setups and looks at how the time evolution
of the passive tracer depends on the advection or transport scheme that is selected 
for the tracer. 

Passive tracers are useful in many numerical experiments. In some cases tracers are
used to track flow pathways, for example in \cite{Dutay02} a passive tracer is used
to track pathways of CFC-11 in 13 global ocean models, using a numerical
configuration similar to the example described in section \ref{sect:eg-offline-cfc}).
In other cases tracers are used as a way
to infer bulk mixing coefficients for a turbulent flow field, for example in 
\cite{marsh06} a tracer is used to infer eddy mixing coefficients in the
Antarctic Circumpolar Current region. In biogeochemical and ecological simulations large numbers 
of tracers are used that carry the concentrations of biological nutrients and concentrations of 
biological species, for example in ....
When using tracers for these and other purposes it is useful to have a feel for the role
that the advection scheme employed plays in determining properties of the tracer distribution.
In particular, in a discrete numerical model tracer advection only approximates the 
continuum behavior in space and time and different advection schemes introduce diferent 
approximations so that the resulting tracer distributions vary. In the following 
text we illustrate how
to use the different advection schemes available in MITgcm here, and discuss which properties 
are well represented by each one. The advection schemes selections also apply to active
tracers (e.g. $T$ and $S$) and the character of the schemes also affect their distributions
and behavior.

\subsection{Advection and tracer transport}

In general, the tracer problem we want to solve can be written

\begin{equation}
\label{EQ:eg-adv-gyre-generic-tracer}
\frac{\partial C}{partial t} = -U \cdot \nabla C + S
\end{equation}

where $C$ is the tracer concentration in a model cell, $U$ is the model three-dimensional
flow field ( $U=(u,v,w)$ ). In (\ref{EQ:eg-adv-gyre-generic-tracer}) $S$ represents source, sink 
and tendency terms not associated with advective transport. Example of terms in $S$ include
(i) air-sea fluxes for a dissolved gas, (ii) biological grazing and growth terms (for a 
biogeochemical problem) or (iii) convective mixing and other sub-grid parameterizations of 
mixing. In this section we are primarily concerned with 
\begin{enumerate}
\item how to introduce the tracer term, $C$, into an integration
\item the different discretized forms of 
the $-U \cdot \nabla C$ term that are available
\end{enumerate}


\subsection{Introducing a tracer into the flow}

 The MITgcm ptracers package (see section \ref{sec:pkg:ptracers} for a more complete discussion
of the ptracers package and section \ref{sec:pkg:using} for a general introduction to MITgcm 
packages) provides pre-coded support for a simple passive tracer with an initial
distribution at simulation time $t=0$ of $C_0(x,y,z)$. The steps required to use this capability
are 
\begin{enumerate}
\item{\bf Activating the ptracers package.} This simply requires adding the line {\tt ptracers} to
the {\tt packages.conf} file in the {\it code/} directory for the experiment.
\end{enumerate}

- activating ptracers
- setting initial distribution

To intro
\subsection{Selecting an advection scheme}

- flags in data and data.ptracers

- overlap width

- CPP GAD\_ALLOW\_SOM\_ADVECT required for SOM case

\subsection{Comparison of different advection schemes}

\begin{enumerate}
\item{Conservation}
\item{Dispersion}
\item{Diffusion}
\item{Positive definite}
\end{enumerate}

\subsection{Code and Parameters files for this tutorial}

The code and parameters for the experiments can be found in the MITgcm example experiments 
directory {\it verification/tutorial\_advection\_in\_gyre/}.


1	cnh	1.10	% $Header: /u/u0/gcmpack/mitgcmdoc/part3/case_studies/advection_in_gyre_circulation/adv_gyre.tex,v 1.9 2008/01/15 22:29:10 cnh Exp $
2	jahn	1.1	% $Name: $
3
4			\bodytext{bgcolor="#FFFFFFFF"}
5
6
7			\section[Gyre Advection Example]{Ocean Gyre Advection Schemes}
8	cnh	1.8	\label{www:tutorials}
9	jahn	1.1	\label{sect:eg-adv-gyre}
10			\begin{rawhtml}
11			<!-- CMIREDIR:eg-adv-gyre: -->
12			\end{rawhtml}
13
14	cnh	1.10	Author: Oliver Jahn and Chris Hill
15
16
17
18	cnh	1.2	This set of examples is based on the barotropic and baroclinic gyre MITgcm configurations,
19	cnh	1.7	that are described in the tutorial sections \ref{sect:eg-baro} and \ref{sect:eg-fourlayer}.
20	cnh	1.4	The examples in this section explain how to introduce a passive tracer into the flow
21	cnh	1.2	field of the barotropic and baroclinic gyre setups and looks at how the time evolution
22			of the passive tracer depends on the advection or transport scheme that is selected
23			for the tracer.
24
25	cnh	1.3	Passive tracers are useful in many numerical experiments. In some cases tracers are
26			used to track flow pathways, for example in \cite{Dutay02} a passive tracer is used
27	cnh	1.4	to track pathways of CFC-11 in 13 global ocean models, using a numerical
28			configuration similar to the example described in section \ref{sect:eg-offline-cfc}).
29	cnh	1.3	In other cases tracers are used as a way
30	cnh	1.4	to infer bulk mixing coefficients for a turbulent flow field, for example in
31			\cite{marsh06} a tracer is used to infer eddy mixing coefficients in the
32			Antarctic Circumpolar Current region. In biogeochemical and ecological simulations large numbers
33			of tracers are used that carry the concentrations of biological nutrients and concentrations of
34			biological species, for example in ....
35	cnh	1.3	When using tracers for these and other purposes it is useful to have a feel for the role
36			that the advection scheme employed plays in determining properties of the tracer distribution.
37	cnh	1.4	In particular, in a discrete numerical model tracer advection only approximates the
38			continuum behavior in space and time and different advection schemes introduce diferent
39			approximations so that the resulting tracer distributions vary. In the following
40			text we illustrate how
41			to use the different advection schemes available in MITgcm here, and discuss which properties
42			are well represented by each one. The advection schemes selections also apply to active
43			tracers (e.g. $T$ and $S$) and the character of the schemes also affect their distributions
44			and behavior.
45	cnh	1.3
46			\subsection{Advection and tracer transport}
47	cnh	1.4
48			In general, the tracer problem we want to solve can be written
49
50			\begin{equation}
51			\label{EQ:eg-adv-gyre-generic-tracer}
52			\frac{\partial C}{partial t} = -U \cdot \nabla C + S
53			\end{equation}
54
55			where $C$ is the tracer concentration in a model cell, $U$ is the model three-dimensional
56			flow field ( $U=(u,v,w)$ ). In (\ref{EQ:eg-adv-gyre-generic-tracer}) $S$ represents source, sink
57			and tendency terms not associated with advective transport. Example of terms in $S$ include
58			(i) air-sea fluxes for a dissolved gas, (ii) biological grazing and growth terms (for a
59			biogeochemical problem) or (iii) convective mixing and other sub-grid parameterizations of
60			mixing. In this section we are primarily concerned with
61			\begin{enumerate}
62			\item how to introduce the tracer term, $C$, into an integration
63			\item the different discretized forms of
64			the $-U \cdot \nabla C$ term that are available
65			\end{enumerate}
66
67
68	cnh	1.10	\subsection{Introducing a tracer into the flow}
69	cnh	1.4
70	cnh	1.9	The MITgcm ptracers package (see section \ref{sec:pkg:ptracers} for a more complete discussion
71			of the ptracers package and section \ref{sec:pkg:using} for a general introduction to MITgcm
72			packages) provides pre-coded support for a simple passive tracer with an initial
73			distribution at simulation time $t=0$ of $C_0(x,y,z)$. The steps required to use this capability
74			are
75			\begin{enumerate}
76	cnh	1.10	\item{\bf Activating the ptracers package.} This simply requires adding the line {\tt ptracers} to
77			the {\tt packages.conf} file in the {\it code/} directory for the experiment.
78	cnh	1.9	\end{enumerate}
79
80	cnh	1.4	- activating ptracers
81			- setting initial distribution
82
83			To intro
84			\subsection{Selecting an advection scheme}
85
86			- flags in data and data.ptracers
87
88			- overlap width
89
90	cnh	1.6	- CPP GAD\_ALLOW\_SOM\_ADVECT required for SOM case
91	cnh	1.4
92			\subsection{Comparison of different advection schemes}
93
94			\begin{enumerate}
95			\item{Conservation}
96			\item{Dispersion}
97			\item{Diffusion}
98			\item{Positive definite}
99			\end{enumerate}
100
101	cnh	1.9	\subsection{Code and Parameters files for this tutorial}
102	cnh	1.10
103			The code and parameters for the experiments can be found in the MITgcm example experiments
104			directory {\it verification/tutorial\_advection\_in\_gyre/}.
105
106	cnh	1.3
107
108
109	cnh	1.2
110	jahn	1.1
111