¥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
conservation of tracers (temperature, salinity)
u hor. velocity w vertical velocity
j tracer
t time
p pressure
r0 density
T temperature
S salinity
hydrostatic in the vertical
equation of state
grid