Spatial Discretization
======================

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.

.. toctree::
    :maxdepth: 2

    api/generated/pages/Discrete_Grids
    api/generated/pages/Finite_Difference_Operators
    api/generated/pages/PPM
    api/generated/pages/Discrete_Coriolis
    api/generated/pages/Discrete_PG
    api/generated/pages/Energetic_Consistency
    api/generated/pages/Discrete_OBC