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Year

A year is the term for any period of time that is derived from the period of the orbit of the Earth (or indeed any planet) around its Sun. In astronomy, several types of year are defined:

  • sidereal year: the actual period for the Earth to complete one revolution of its orbit, as measured in a fixed frame of reference (such as the fixed stars, Latin sidus). Its duration is on average:
365.256363051 days (at the epoch J2000 = 1 Jan. 2000 12h TT).

The actual duration varies from year to year because the motion of the Earth is influenced by the gravity of the Moon and other planets.

  • tropical year: the period for the Earth to complete one revolution with respect to the framework provided by the intersection of the ecliptic (the plane of the orbit of the Earth) and the plane of the equator (the plane perpendicular to the rotation axis of the Earth). Because of the precession, this framework moves slowly backwards along the ecliptic with respect to the fixed stars; as a consequence, the Earth completes this year before it completes a full orbit as measured in a fixed reference frame. Therefore a tropical year is shorter than the sidereal year: its duration (averaged over all tropical ecliptic points) was:
365.24218967 days (365d 5h 48m 45s) (at the epoch J2000).

 

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