To account for a generalized variation in cell thickness, a factor of dhui,k,j must be included in horizontal diffusive and advective operators. The following equations should be compared with the corresponding set in Section 21.3.1:
where the horizontal viscous fluxes on U-cell faces become
| = | ![]() |
(26.6) | |
| = | (26.7) |
Because the lateral boundary condition is no-flux for
tracers but no-slip for velocity, the horizontal viscosity
has zonal and meridional
components given by
where Am is the lateral viscosity coefficient26.2. The above form differs from Bryan (1969) due to the
inclusion of effective cell face heights
and
and a sink term due to a no-slip lateral boundary
condition given by
which is zero where U-cell thickness is constant (i.e.
)
within a vertical level but acts effectively as a
bottom drag
| (26.13) |
where U-cell thickness varies within a vertical level. The
constant of proportionality (
)
represents
the fraction of cell face height over which a no-slip condition is
applied.
There is no change in the form of the horizontal advective
flux given by Equations (22.86) and
(22.87) because advective velocities
and
absorb a factor
dhui,k,jand become advective transports given by Equations (26.40)
and (26.41). Horizontal advective velocities for the U-cells
are then given by Equations (22.22) and (22.21).
The only change in the vertical advective and vertical diffusive
operators is to replace dztk in the vertical derivative with
dhui,k,j. When defining vertical fluxes at the bottom cell faces,
dhwk in the vertical derivatives is replaced by
.