The Model (3)
•Vertical Coordinates
–Hybrid coordinates
•Nearsurface: z-coordinates
•Shallow water: sigma (terrain-following) coordinates
•Coordinates are isopycnic in the bulk of the ocean interior
–Isopycnic coordinates (MICOM mode)
•Hybrid Vertical Coordinate Scheme (part 1)
–In the open ocean, the coordinates are isopycnic except year the surface where minimum coordinate separation is enforced. The minimum separation differs for each layer, giving the user great flexibility to set the vertical coordinate structure in the z-coordinate domain.
–A cushion function described in Bleck and Benjamin (1993) provides a smooth transition between the isopycnic and z-coordinate domains.
–To activate the sigma coordinate domain, the user specifies the number of sigma coordinates n and the coordinate separation d. Vertical coordinates become terrain-following where bottom depth is less than n*d. In extremely shallow water, the coordinates revert to level coordinates.