/[MITgcm]/manual/s_examples/global_oce_latlon/climatalogical_ogcm.tex
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revision 1.4 by adcroft, Tue Nov 13 18:19:18 2001 UTC revision 1.7 by adcroft, Tue Nov 13 20:13:54 2001 UTC
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2  % $Name$  % $Name$
3    
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"}
8    
# Line 148  $ Line 148  $
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
# Line 210  g\rho_{0} \eta + \int^{0}_{-z}\rho^{'} d Line 210  g\rho_{0} \eta + \int^{0}_{-z}\rho^{'} d
210  $v=\frac{Dy}{Dt}=r \frac{D \phi}{Dt}$  $v=\frac{Dy}{Dt}=r \frac{D \phi}{Dt}$
211  are the zonal and meridional components of the  are the zonal and meridional components of the
212  flow vector, $\vec{u}$, on the sphere. As described in  flow vector, $\vec{u}$, on the sphere. As described in
213  MITgcm Numerical Solution Procedure \cite{MITgcm_Numerical_Scheme}, the time  MITgcm Numerical Solution Procedure \ref{chap:discretization}, the time
214  evolution of potential temperature, $\theta$, equation is solved prognostically.  evolution of potential temperature, $\theta$, equation is solved prognostically.
215  The total pressure, $p$, is diagnosed by summing pressure due to surface  The total pressure, $p$, is diagnosed by summing pressure due to surface
216  elevation $\eta$ and the hydrostatic pressure.  elevation $\eta$ and the hydrostatic pressure.
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