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Next: 26.2.2.2 Computing density in Up: 26.2.2 Pressure gradient Previous: 26.2.2 Pressure gradient

   
26.2.2.1 Example where density varies linearly with depth

If density varies linearly with depth, then


\begin{displaymath}\delta_z(\rho_{i,k,j}) = constant
\end{displaymath} (26.24)

and density $\rho_{i,k,j}$ can be expanded in terms of density in the upper level $\rho_{i,k-1,j}$ as


 \begin{displaymath}\rho_{i,k,j} = \rho_{i,k-1,j} + \delta_z{\rho_{i,k-1,j}}\cdot dhw_{i,k-1,j} \;.
\end{displaymath} (26.25)

Using the above expansion to eliminate $\rho_{i,k,j}$ in Equation (26.24) results in the following expansions:


$\displaystyle \delx(\rho_{i,k,j})$ = $\displaystyle \delta_z (\rho_{i,k-1,j})\cdot \delx (zt_{i,k,j})$ (26.26)
$\displaystyle \overline{\rho_{i,k,j}}^\lambda$ = $\displaystyle \rho_{i,k-1,j} + \delta_z (\rho_{i,k-1,j}) \cdot \overline{dhw_{i,k-1,j}}^\lambda \;.$ (26.27)

Substituting the above expansions into Equation (26.24) results in


$\displaystyle {\cal P}_x(k) = 0$     (26.28)



RC Pacanowski and SM Griffies, GFDL, Jan 2000