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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:
- age
- ocean_uptake
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.