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