The model equations are the layer-integrated vector-invariant form of the hydrostatic primitive equations (either Boussinesq or non-Boussinesq).
We present the equations starting from the hydrostatic Boussinesq equation in height coordinates and progress through vector-invariant and general-coordinate equations to the final equations used in the A.L.E. algorithm, taken from .
- Notation for equations
- Governing Equations
- General coordinate equations