/[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 1.5 by adcroft, Tue Nov 13 18:22:24 2001 UTC
# 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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