¥Bryan-Cox type model, z-level
vertical grid, finite difference model
Parallel Ocean Program (POP)
conservation
of mass for incompressible fluid
conservation
of momentum
advection
diffusion
advection
diffusion
Coriolis
pressure
gradient
conservation
of tracers (temperature, salinity)
u
hor. velocity wvertical
velocity
hor. velocity wvertical
velocityjtracer
tracerttime
timeppressure
pressurer0density
densityTtemperature
temperatureSsalinity
salinityhydrostatic
in the vertical
equation
of state
grid
source/
sink