/[MITgcm]/manual/s_algorithm/text/nonlin_frsurf.tex
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revision 1.4 by adcroft, Wed Sep 26 20:19:52 2001 UTC revision 1.5 by cnh, Thu Oct 25 18:36:53 2001 UTC
# Line 31  upper surface, $R_o = 0$, is essentially Line 31  upper surface, $R_o = 0$, is essentially
31  easily be incorporated in $\Phi'_{hyd}$.  easily be incorporated in $\Phi'_{hyd}$.
32    
33  For the atmosphere, however, because of topographic effects, the  For the atmosphere, however, because of topographic effects, the
34  reference surface pressure $R_o$ has large spacial variations that  reference surface pressure $R_o$ has large spatial variations that
35  are responsible for significant $b_s$ variations (from 0.8 to 1.2  are responsible for significant $b_s$ variations (from 0.8 to 1.2
36  $[m^3/kg]$). For this reason, we use a non-uniform linear coefficient  $[m^3/kg]$). For this reason, we use a non-uniform linear coefficient
37  $b_s$.  $b_s$.
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