/[MITgcm]/MITgcm_contrib/articles/ceaice/ceaice_forward.tex
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revision 1.2 by dimitri, Wed Feb 27 21:50:42 2008 UTC revision 1.3 by dimitri, Thu Feb 28 15:12:57 2008 UTC
# Line 39  The ocean model is coupled to the sea-ic Line 39  The ocean model is coupled to the sea-ic
39  Section~\ref{sec:model} with the following specific options.  The  Section~\ref{sec:model} with the following specific options.  The
40  zero-heat-capacity thermodynamics formulation of \citet{hib80} is used to  zero-heat-capacity thermodynamics formulation of \citet{hib80} is used to
41  compute sea ice thickness and concentration.  Snow cover and sea ice salinity  compute sea ice thickness and concentration.  Snow cover and sea ice salinity
42  are prognostic.    are prognostic.  Open water, dry ice, wet ice, dry snow, and wet snow albedo
43    are, respectively, 0.15, 0.88, 0.79, 0.97, and 0.83. Ice mechanics follow the
44    viscous plastic rheology of \citet{hibler79} and the ice momentum equation is
45    solved numerically using the C-grid implementation of the \citet{zha97} LSR
46    dynamics model discussed hereinabove.
47    
48  Ice mechanics follow the viscous plastic rheology of  This particular ECCO2 simulation is initialized from temperature and salinity
49  \citet{hibler79} and the ice momentum equation is solved numerically using the  fields derived from the
 C-grid implementation of the \citet{zha97} LSR dyanmics model discussed  
 hereinabove.  
50    
 Open water, dry  
 ice, wet ice, dry snow, and wet snow albedo are, respectively, 0.15, 0.85,  
 0.76, 0.94, and 0.8.  
   
 \subsection{Arctic Domain with Open Boundaries}  
 \label{sec:arctic}  
51    
52    
53  \subsection{Arctic Domain with Open Boundaries}  \subsection{Arctic Domain with Open Boundaries}
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