Next: 8.3 Surface tracer flux
Up: 8. The tracer budget
Previous: 8.1 The continuum tracer
8.2 Finite volume budget for the total tracer
The time tendency for the total amount of tracer in a cell is given by
![$\displaystyle \partial_{t} [ [T]_k ]$](s2img527.gif) |
= |
![$\displaystyle [ [T_{t} ]_k ] + [T(\eta) \,\eta_{t}] \, \delta_{k1},$](s2img528.gif) |
(8.2) |
where the square brackets denote volume integration. For example,
within the Boussinesq approximation, the volume integral of
represents the total mass of salt within this
volume. Likewise, the volume integral of
represents the total heat (in units of energy) within this
volume. For T representing the mass/volume of a passive tracer,
the volume integral of T is the total mass of this tracer in the
volume.
The first term on the right hand side of equation
(8.2) arises from the time tendency of the
tracer concentration inside the box. The second term occurs only for
a surface cell and comes from the time tendency of the surface height
multiplied by the surface tracer concentration. This term alters the
tracer budget through changing the volume of the box, and it is
absent in the rigid lid approximation for which
.
Note
that the value of the tracer in this expression is that at the ocean
side of the free surface
.
Use of the surface kinematic boundary condition
(7.16) brings the tracer budget
equation (8.2) to the form
![$\displaystyle \partial_{t} [ [T]_k ]$](s2img527.gif) |
= |
![$\displaystyle \left[ [-\nabla \cdot ({\bf u}T + {\bf F} ) ]_k \right]
+
\left[ ...
...( w + q_{w} - {\bf u}_{h} \cdot \nabla_{h} \eta \right) \right] \, \delta_{k1},$](s2img530.gif) |
(8.3) |
where all the terms multiplying
are evaluated at
.
Integration by parts leads to
![$\displaystyle [ [ \nabla_{h} \cdot ({\bf u}_{h} \, T + {\bf F}_{h} ) ]_k ]$](s2img532.gif) |
= |
![$\displaystyle [ \nabla_{h} \cdot [ {\bf u}_{h} \, T + {\bf F}_{h} ]_k ]
- [ \nabla_{h} \eta \cdot ({\bf u}_{h} \, T + {\bf F}_{h} ) ] \, \delta_{k1},$](s2img533.gif) |
(8.4) |
where again the terms multiplying
are evaluated at
.
Using this result in equation (8.3) brings
about a cancellation of the
term appearing in the
part of the budget. The vertical
divergence integrates to
![$\displaystyle [ [ \partial_{z} \, (w \, T + F^{z}) ]_k ]$](s2img535.gif) |
= |
![$\displaystyle [ (w \, T + F^{z})_{z=z_{k-1}} - (w \, T + F^{z})_{z=z_{k}} ],$](s2img536.gif) |
(8.5) |
which is the divergence of the area integrated flux across the
horizontal cell faces. These results render
For a surface cell with k=1, there is a cancellation of the
term to yield the budget
![$\displaystyle \partial_{t}
[ [T]_{k=1} ]$](s2img540.gif) |
= |
![$\displaystyle - [ \nabla_{h} \cdot [ {\bf u}_{h} \, T + {\bf F}_{h} ]_k ]
+ [(w...
...{z=z_{1}} +
(q_{w} \, T - F^{z} + \nabla_{h} \eta \cdot {\bf F}_{h})_{z=\eta} ]$](s2img541.gif) |
(8.7) |
Next: 8.3 Surface tracer flux
Up: 8. The tracer budget
Previous: 8.1 The continuum tracer
RC Pacanowski and SM Griffies, GFDL, Jan 2000