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Revision 1 as of 2008-01-11 10:55:01
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Revision 17 as of 2019-07-31 12:25:07
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Editor: NicoleThomas
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Deletions are marked like this. Additions are marked like this.
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#format inline_latex #acl ClamsUserGroup:read,write,delete,revert All:read
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The 2D (isentropic) and 3D mixing in CLaMS is implemented in the FORTRAN-90 program '''["mix.f90"]'''. The handling of the boundary conditions is controlled by the program '''["bmix.f90"]'''.
For the description of the 2D/3D mixing algorithm, see [2,1]
The 2D (isentropic) and 3D mixing in CLaMS is implemented in the FORTRAN-90 program '''[[/mix.f90 | mix.f90]]'''. <<BR>>
The handling of the boundary conditions is controlled by the program '''[[/bmix.f90 | bmix.f90]]'''. <<BR>>
For the description of the 2D/3D mixing algorithm, see ''References''.

Utility progams in package mix:
 * age
 * [[ /clams2boundary | clams2boundary ]]
 * ocean_uptake
 * [[ /replace_lbound | replace_lbound ]]
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{{{#!latex
\begin{thebibliography}{1}
\bibitem{Konopka2004}
P.~Konopka, H.-M. Steinhorst, J.-U. Groo\ss, G.~G\"unther, R.~M\"{u}ller, J.~W.
  Elkins, H.-J. Jost, E.~Richard, U.~Schmidt, G.~Toon, and D.~S. McKenna.
\newblock Mixing and ozone loss in the 1999-2000 arctic vortex: {S}imulations
  with the 3-dimensional {Chemical Lagrangian Model of the Stratosphere
  (CLaMS)}.
\newblock {\em J. Geophys. Res.}, 109(D2):doi:10.1029/2003JD003792, 2004.
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\bibitem{McKenna2002a}
D.~S. {McKenna}, P.~Konopka, J.-U. Groo\ss, G.~G\"unther, R.~M\"uller,
  R.~Spang, D.~Offermann, and Y.~Orsolini.
\newblock A new {C}hemical {L}agrangian {M}odel of the {S}tratosphere
  {(CLaMS)}: {P}art {I} {F}ormulation of advection and mixing.
\newblock {\em J. Geophys. Res.}, 107(D16):4309, doi:10.1029/2000JD000114,
  2002.
\end{thebibliography}
}}}
=== References ===

P.Konopka, H.-M.Steinhorst, J.-U.Grooß, G.Günther, R.Müller, J.W.Elkins, H.-J.Jost, E.Richard, U.Schmidt, G.Toon, and D.S.McKenna. Mixing and ozone loss in the 1999-2000 arctic vortex: Simulations with the 3-dimensional Chemical Lagrangian Model of the Stratosphere (CLaMS). ''J. Geophys. Res.'', 109(D2):doi:10.1029/2003JD003792, 2004.

D.S.McKenna, P.Konopka, J.-U.Grooß, G.Günther, R.Müller, R.Spang, D.Offermann, and Y.Orsolini. A new Chemical Lagrangian Model of the Stratosphere (CLaMS): Part I Formulation of advection and mixing. ''J. Geophys. Res.'', 107(D16):4309, doi:10.1029/2000JD000114, 2002.

----

[[/Changes|History of Changes]]

The package mix

The 2D (isentropic) and 3D mixing in CLaMS is implemented in the FORTRAN-90 program mix.f90.
The handling of the boundary conditions is controlled by the program bmix.f90.
For the description of the 2D/3D mixing algorithm, see References.

Utility progams in package mix:

References

P.Konopka, H.-M.Steinhorst, J.-U.Grooß, G.Günther, R.Müller, J.W.Elkins, H.-J.Jost, E.Richard, U.Schmidt, G.Toon, and D.S.McKenna. Mixing and ozone loss in the 1999-2000 arctic vortex: Simulations with the 3-dimensional Chemical Lagrangian Model of the Stratosphere (CLaMS). J. Geophys. Res., 109(D2):doi:10.1029/2003JD003792, 2004.

D.S.McKenna, P.Konopka, J.-U.Grooß, G.Günther, R.Müller, R.Spang, D.Offermann, and Y.Orsolini. A new Chemical Lagrangian Model of the Stratosphere (CLaMS): Part I Formulation of advection and mixing. J. Geophys. Res., 107(D16):4309, doi:10.1029/2000JD000114, 2002.


History of Changes

mix (last edited 2019-07-31 12:25:07 by NicoleThomas)