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4.2 The primitive equations

The continuous equations solved by MOM are given by


       
ut = $\displaystyle - \nabla \cdot (u \, {\bf u}) + v \left(f + \frac{u\tan\phi}{a} \...
...ac{1}{a \, \rho_\circ \cdot \cos\phi} \right) p_\lambda
+ (\kappa_mu_z)_z + F^u$ (4.1)
       
vt = $\displaystyle - \nabla \cdot (v \, {\bf u}) - u \left(f + \frac{u\tan\phi}{a} \right)
-\left(\frac{1}{a \, \rho_\circ}\right) p_\phi
+ (\kappa_mv_z)_z + F^v$ (4.2)
       
wz = $\displaystyle - \nabla_{h} \cdot {\bf u}_{h}$ (4.3)
       
pz = $\displaystyle -\rho \, g$ (4.4)
       
$\displaystyle \theta_t$ = $\displaystyle - \nabla \cdot [ {\bf u} \, \theta + {\bf F}(\theta) ]$ (4.5)
       
st = $\displaystyle - \nabla \cdot [ {\bf u} \, s + {\bf F}(s)]$ (4.6)
       
$\displaystyle \rho$ = $\displaystyle \rho(\theta,s,z).$ (4.7)

The coordinate $\phi $ is latitude, which increases northward and is zero at the equator. $\lambda $ is longitude, which increases eastward with zero defined at an arbitrary longitude (e.g., Greenwich, England). z is the vertical coordinate, which is positive upwards and zero at the surface of a resting ocean. Boldface characters represent vector quantities.



 
next up previous contents
Next: 4.2.1 Basic constants and Up: 4. Fundamental equations Previous: 4.1 Assumptions
RC Pacanowski and SM Griffies, GFDL, Jan 2000