### precession

(periodic change in a body's rotation or orbit)

**Precession** is a periodic change in a body's rotation or orbit.
The Earth's rotation precesses the direction that the poles point,
aligning most closely with different stars as the precession progresses
(the **precession of the equinoxes**).
In the case of planets or moons this type of
precession is called **axial precession**.
Earth's precession rate (**precession constant**) is about 1/26000 years.
This is caused by the effect of the Sun's gravity
on the Earth's tilted rotation axis as well as similar
effects from the Moon and Jupiter, and from the
Earth's orbital eccentricity.

An orbit's precession, an example of something other than axial precession,
could be its apoapsis shifting to different directions over time.

Other spinning objects besides astronomical bodies can precess,
such as a spinning top's axis of rotation rotating so that its
point at the top of the top moves in a circular path.

Determining a planet's (axial) precession constant allows
its **moment of inertia** to be calculated. For
the effects of its star (much more massive than the
planet), a formula is:

Ω = (-3/2)((C-A)/C)(Gm/a^{3})(1/ω)cos β

- Ω - precession rate.
- C - planet's
**polar moment of inertia** (i.e., due its equatorial bulge), essentially what we are after.
- A - planet's moment of inertia around any equatorial diameter, presumed to be well-estimated from mass and radius of a near-sphere.
- m - star's mass.
- G - gravitational constant.
- a - distance from star to planet.
- ω - planet's rotation rate (day).
- β - angle between planet's orbital plane and the plane of its equator.

(*orbits,rotation,kinematics*)
http://en.wikipedia.org/wiki/Apsidal_precession

http://en.wikipedia.org/wiki/Axial_precession

**Referenced by:**

epoch

equatorial coordinate system

equinox

nutation

orbital resonance

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