as well as the evolution equations for the potential temperature 6 and salinity S:

where p0 is the reference density of sea water; kM and kH are coefficients of the vertical and horizontal eddy exchange; F; and F^ are the zonal and meridional components of the frictional force (they are calculated using a linearized version of appropriate formulae for the atmospheric submodel);

d() = i()+ +8v^COS(p + lw( ), df dt a cos (p dX a cos cp dcp dz

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