Next: 42.2 Horizontal-vertical diffusion
Up: 42.1 Basic properties
Previous: 42.1.1.2 Skew or anti-symmetric
Multiplying the tracer equation
 |
(42.23) |
by TN-1, where N is some positive integer, yields
 |
= |
 |
(42.24) |
| |
= |
 |
(42.25) |
| |
= |
 |
(42.26) |
The time tendency is therefore given by
where the flux
| Fm |
= |
 |
(42.29) |
| |
= |
 |
(42.30) |
| |
 |
FmK + FmA |
(42.31) |
was introduced. Note that the above steps assumed a divergence-free
velocity field (
)
and the identity
(B.7) (
)
was
employed.
Integrating the previous equation over some domain yields
![\begin{displaymath}\partial_{t} \int d\vec{x} \; T^{N} =
\int d\vec{x} \; \lef...
... - N(N-1)T^{N-2} K^{m n} \partial_{m}T \partial_{n}T \right].
\end{displaymath}](s9img308.gif) |
(42.32) |
Stokes' Theorem brings this expression to
 |
(42.33) |
where
is the outward normal to the boundary. Assuming the
normal velocity vanishes at the domain boundary (
)
yields for the time tendency of the globally integrated
N'th tracer moment
 |
(42.34) |
It is of interest to consider some special cases. First, consider
the case with no diffusive mixing, which means there is a zero
symmetric component to the tracer mixing tensor (
Km n = FmK
= 0). Therefore, all moments of the tracer are conserved when there
is no normal skew flux at the boundaries (
), or equivalently there is zero normal induced velocity
(
)
at the boundaries. For example, the
skew flux associated with the Gent-McWilliams effective transport
velocity satisfies these conditions and so preserves all tracer moments
(Gent and McWilliams 1990).
For the case with zero anti-symmetric but nonzero symmetric tracer
mixing tensor, the first moment, or the total tracer, is conserved in
source free regions where there is no tracer flux normal to the
boundary; i.e., if
at the domain boundaries. In the absence of
sources, the tracer's second moment satisfies the evolution equation
 |
(42.35) |
Therefore, this mixing tensor dissipates the tracer variance
42.2 over the
source-free domain if the tensor Km n is a positive semi-definite
tensor (i.e., the right hand side is negative semi-definite if Km
n is positive semi-definite). This property of diffusion is
fundamental, and is taken as the foundation for the numerical
discretization of isopycnal diffusion in MOM. All higher moments of
the tracer are also dissipated by diffusion assuming the usual case of
a non-negative tracer concentration.
Next: 42.2 Horizontal-vertical diffusion
Up: 42.1 Basic properties
Previous: 42.1.1.2 Skew or anti-symmetric
RC Pacanowski and SM Griffies, GFDL, Jan 2000