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9.4.8 Summary of second order friction
The fundamental assumptions that determine the form of the momentum
friction are the following:
- Horizontal kinetic energy is dissipated by the friction.
- The friction does not introduce interior sources or sinks of
angular momentum.
- The fluid motion is quasi-hydrostatic.
- The friction exhibits lateral or transverse isotropy in which
gravity picks out the only special direction.
Each of these properties is satisfied by the following two components
to the friction
| |
|
 |
(9.126) |
| |
|
 |
(9.127) |
With the Boussinesq approximation, the factors of density are
formally replaced by the constant
,
and so cancel out from
these expressions. The metric tensor is assumed to be diagonal and
to define the infinitesimal distance between two points as
 |
(9.128) |
In this expression, the metric components
g11 = h12 and
g22 = h22 are functions only of the transverse
coordinates, and the physical displacements
| d x |
= |
 |
(9.129) |
| d y |
= |
 |
(9.130) |
have dimensions of length. The corresponding physical components of
the partial derivative operators
bring the horizontal tension to the form
 |
(9.133) |
and the horizontal shearing strain
 |
(9.134) |
DT and DS are generically called the deformation rates, and
the each have dimensions of t-1. In spherical coordinates,
,
,
h2
= a, and
,
.
The
viscosity A is generally a function of the fluid flow, and it has
dimension L2/t. The generalized curvilinear coordinates x,y,z are physical components, and so each has dimension of length.
Likewise, the corresponding physical velocity components (u,v,w) have dimension L/t.
Next: 9.5 Biharmonic friction
Up: 9.4 Orthogonal curvilinear coordinates
Previous: 9.4.7 Effects on kinetic
RC Pacanowski and SM Griffies, GFDL, Jan 2000