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Next: 2.14.4 Non-hydrostatic metric terms
Up: 2.14 Flux-form momentum equations
Previous: 2.14.2 Coriolis terms
Contents
The most commonly used coordinate system on the sphere is the
geographic system
. The curvilinear nature of these
coordinates on the sphere lead to some ``metric'' terms in the
component momentum equations. Under the thin-atmosphere and
hydrostatic approximations these terms are discretized:
 |
 |
 |
(2.113) |
 |
 |
 |
(2.114) |
 |
 |
0 |
(2.115) |
where
is the radius of the planet (sphericity is assumed) or the
radial distance of the particle (i.e. a function of height). It is
easy to see that this discretization satisfies all the properties of
the discrete Coriolis terms since the metric factor
can be viewed as a modification of the vertical Coriolis
parameter:
.
However, as for the Coriolis terms, a non-energy conserving form has
exclusively been used to date:
where
is evaluated at the
and
points
respectively.
Next: 2.14.4 Non-hydrostatic metric terms
Up: 2.14 Flux-form momentum equations
Previous: 2.14.2 Coriolis terms
Contents
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Massachusetts Institute of Technology |
Last update 2011-01-09 |
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