/[MITgcm]/manual/s_examples/barotropic_gyre/baro.tex
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revision 1.5 by adcroft, Tue Nov 13 18:19:18 2001 UTC revision 1.7 by adcroft, Tue Nov 13 20:13:54 2001 UTC
# Line 2  Line 2 
2  % $Name$  % $Name$
3    
4  \section{Example: Barotropic Ocean Gyre In Cartesian Coordinates}  \section{Example: Barotropic Ocean Gyre In Cartesian Coordinates}
5  \label{sec:eg-baro}  \label{sect:eg-baro}
6    
7  \bodytext{bgcolor="#FFFFFFFF"}  \bodytext{bgcolor="#FFFFFFFF"}
8    
# Line 82  walls at $x=$~0,1200km and at $y=$~0,120 Line 82  walls at $x=$~0,1200km and at $y=$~0,120
82    
83  \subsection{Equations Solved}  \subsection{Equations Solved}
84  The model is configured in hydrostatic form. The implicit free surface form of the  The model is configured in hydrostatic form. The implicit free surface form of the
85  pressure equation described in Marshall et. al \cite{Marshall97a} is  pressure equation described in Marshall et. al \cite{marshall:97a} is
86  employed.  employed.
87  A horizontal Laplacian operator $\nabla_{h}^2$ provides viscous  A horizontal Laplacian operator $\nabla_{h}^2$ provides viscous
88  dissipation. The wind-stress momentum input is added to the momentum equation  dissipation. The wind-stress momentum input is added to the momentum equation
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