/[MITgcm]/manual/s_examples/global_oce_latlon/climatalogical_ogcm.tex
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revision 1.5 by adcroft, Tue Nov 13 18:22:24 2001 UTC revision 1.7 by adcroft, Tue Nov 13 20:13:54 2001 UTC
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2  % $Name$  % $Name$
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4  \section{Example: 4$^\circ$ Global Climatological Ocean Simulation}  \section{Example: 4$^\circ$ Global Climatological Ocean Simulation}
5  \label{sec:eg-global}  \label{sect:eg-global}
6    
7  \bodytext{bgcolor="#FFFFFFFF"}  \bodytext{bgcolor="#FFFFFFFF"}
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148   \Delta z_{20}=815\,{\rm m}   \Delta z_{20}=815\,{\rm m}
149  $ (here the numeric subscript indicates the model level index number, ${\tt k}$).  $ (here the numeric subscript indicates the model level index number, ${\tt k}$).
150  The implicit free surface form of the pressure equation described in Marshall et. al  The implicit free surface form of the pressure equation described in Marshall et. al
151  \cite{Marshall97a} is employed. A Laplacian operator, $\nabla^2$, provides viscous  \cite{marshall:97a} is employed. A Laplacian operator, $\nabla^2$, provides viscous
152  dissipation. Thermal and haline diffusion is also represented by a Laplacian operator.  dissipation. Thermal and haline diffusion is also represented by a Laplacian operator.
153    
154  Wind-stress forcing is added to the momentum equations for both  Wind-stress forcing is added to the momentum equations for both
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