Figure: The physics of the Earth's axial precession
Caption: How the Earth's equatorial bulge and Earth's axial rotation leads to the axial precession.
Further explication:
The oblateness is NOT very large: the Earth equatorial radius R_eq_⊕ = 6378.1 km and the Earth polar radius R_po_⊕ = 6356.8 km: the difference is only 21.3 km (see Wikipedia: Earth Table; Wikipedia: Earth: Shape; Wikipedia: Earth's radius). The flattening ratio is
The differential gravitational force, in fact, the tidal force.
For example, people sometimes talk of torquing a screw.
The oscillation might be damped out in in time due to other perturbations leading to approximate alignment of the Earth's axis and the ecliptic axis.
The Earth's rotation is the cause of the equatorial bulge via the centrifugal force as aforesaid.
However, the situation is somewhat similar to why orbiting objects do NOT fall inward
under gravity.
They keep falling, but keep missing because they have
a sideways motion or, in physics
terminology, angular momentum
(which is a measure of
rotation).
Similarly, the
axis
of rotating Earth
keeps trying to align perpendicular to the direction of
gravity,
but keeps missing because the
Earth has
angular momentum about its
axis
The "missing" is the
axial precession.
For example,
precession
is exhibited by toy tops.
See the figure below
(local link /
general link: precession_toy_top.html).
php require("/home/jeffery/public_html/astro/celestial_sphere/axial_precession.html");?>
php require("/home/jeffery/public_html/astro/mechanics/precession_toy_top.html");?>
Credit and file tracking information follows to the divider line:
Credit/Permission: © David Jeffery, 2003 / Own work.