When vertical thickness of cells is a function of
,
,
and depth, extra terms are needed to construct the change in kinetic
energy due to pressure forces. Multiplying the zonal pressure gradient
given in Equation (26.14) by u and the meridional pressure
gradient given in Equation (26.15) by v and integrating over the
entire ocean volume yields the change in kinetic energy. The finite
difference equivalent of this expression is
where the velocity cell volume element is
| (26.37) |
Note that there are four terms in Equation (26.38). The first two are similar to Equation (A.89) except that dztk in the U-cell volume element has been replaced by dhui,k,j which is the vertical thickness of a U-cell as given by Equation (26.1).
The reduction of Equation (26.38) is similar to the one given for Equation (A.89) except for differences needed to account for spatial dependence of dhui,k,j. In Equation (A.91), dztk must be removed and dhui,k,j is placed inside both derivatives with subscripts matching those on the velocity. In Equation (A.92), dztk is eliminated and dhui,k,j is placed inside both averages with subscripts matching those on the velocity. The horizontal advective velocites become advective transports defined as
but the vertical advective velocities remain as velocities and the continuity equation becomes
which leads to a change in kinetic energy given by
Note that thickness factor dzwk-1 in Equation (A.99) has been replaced by its spatially dependent counterpart dhwi,k-1,j which is the vertical distance between grid points within cells Ti,k,j and Ti,k-1,j. The change in kinetic energy due to the third and fourth terms is given next.