Basic Concepts
Precession Of The Equinoxes
Documentation for Precession Of The Equinoxes
Precession of the Equinoxes
The line of equinoxes is the line where the plane of the Earth’s orbit intersects the plane of the Earth’s equator. The vernal equinox is the point where the Sun, traveling around the Ecliptic, crosses the celestial equator from south to north, around March 21st every year. The vernal equinox defines the zero point of both right ascension (for equatorial coordinates) and longitude (for ecliptic coordinates).
Unfortunately, the Earth’s polar axis shifts very slowly, in a roughly-circular motion around the north ecliptic pole, over a period of about 26,000 years. This motion is called the precession of the equinoxes or just precession. As a result of precession, the vernal equinox slowly creeps around the Ecliptic over the same 26,000-year period. Thus the equatorial and ecliptic coordinates of the stars slowly shift over time, and different stars are seen near the celestial poles.