Ephemeris time

Ephemeris Time (ET) is a time scale used in ephemerides of celestial bodies, in particular the Sun (as observed from the Earth), Moon, planets, and other members of the solar system. This is distinct from Universal Time (UT): the time scale based on the rotation of the Earth around its axis. ET was replaced with the two time scales Terrestrial Dynamical Time (TDT) and Barycentric Dynamical Time (TDB) by the International Astronomical Union (IAU) in 1976. TDT was renamed Terrestrial Time (TT) in 1991.

In the late nineteenth century it was found that the rotation of the Earth ("i.e." the length of the day) was both irregular on short time scales, and was slowing down on longer time scales. In fact, observing the position of the Moon, Sun and planets and comparing this with their ephemerides was a better way to determine the time.

Using the ephemerides based on the theory of the apparent motion of the Sun by Simon Newcomb (1898), the SI second was defined in 1960 as:

:the fraction 1/31,556,925.9747 of the tropical year for 1900 January 0 at 12 hours ephemeris time.

Caesium atomic clocks became operational in 1955, and quickly made it evident that the rotation of the earth fluctuated randomly. This confirmed the utter unsuitability of the mean solar second of Universal Time as a measure of time interval. After three years of comparisons with lunar observations it was determined that the ephemeris second corresponded to 9,192,631,770 cycles of the caesium resonance. Between 1960 and 1984fact|date=September 2007 the length of the SI second was defined to be equal to the ephemeris second.


In 1976 the IAU resolved that the theoretical basis for Ephemeris Time is wholly non-relativistic, and therefore, beginning in 1984 Ephemeris Time would be replaced by the two relativistic timescales based on Dynamical time scale, the Barycentric Dynamical Time (TDB) and Terrestrial Dynamical Time (TDT). For practical purposes the length of the ephemeris second can be taken as equal to the length of the TDB or TDT second.

The difference between ET and UT is called ΔT; it changes irregularly, but the long-term trend is parabolic, decreasing from ancient times until the nineteenth century, and has been increasing at about 0.7 seconds per year since (see leap seconds). International Atomic Time (TAI) was set equal to UT2 at 1 January 1958 0:00:00 . At that time, ΔT was already about 32.18 seconds. The difference between Terrestrial Time (TT) (the successor to ephemeris time) and atomic time was later defined as follows:

:1977 January 1.0003725 TT = 1977 January 1.0000000 TAI, "i.e."

:ET - TAI = 32.184 seconds

This difference may be assumed constant—the rates of TT and TAI are designed to be identical.


* P.K.Seidelmann (ed.), "Explanatory Supplement to the Astronomical Almanac." University Science Books, CA, 1992 ; ISBN 0-935702-68-7

Wikimedia Foundation. 2010.

Look at other dictionaries:

  • ephemeris time — Astron. time measured by the orbital movements of the earth, the moon, and the planets. [1945 50] * * * ▪ chronology       (ET), the first dynamical time scale in history; it was defined by the International Astronomical Union in the 1950s and… …   Universalium

  • ephemeris time — efemeridinis laikas statusas T sritis Standartizacija ir metrologija apibrėžtis Tolygiai tekantis laikas, vartojamas kaip nepriklausomas kintamasis dangaus kūnų mechanikos lygtyse. Jo ir pasaulinio laiko skirtumas tikrinamas stebint Mėnulio… …   Penkiakalbis aiškinamasis metrologijos terminų žodynas

  • ephemeris time — The uniform measure of time defined by the laws of dynamics and determined in principle from the orbital motions of the planets, specifically the orbital motion of the earth as represented by Newcomb’s Tables of the Sun. An ephemeris day equals… …   Aviation dictionary

  • ephemeris time — /əˈfɛmərəs taɪm/ (say uh femuhruhs tuym) noun Astronomy a measure of time independent of variations in the earth s rotation rate. The ephemeris second is the fundamental unit and is defined as a precise fraction of the tropical year 1900 …   Australian English dictionary

  • ephemeris time — noun (astronomy) a measure of time defined by Earth s orbital motion; terrestrial time is mean solar time corrected for the irregularities of the Earth s motions • Syn: ↑terrestrial time, ↑TT, ↑terrestrial dynamical time, ↑TDT • Topics:… …   Useful english dictionary

  • ephemeris time — noun a) A former standard astronomical time scale intended to overcome the drawbacks of irregularly fluctuating mean solar time, superseded in the 1970s. b) A modern relativistic coordinate time scale …   Wiktionary

  • ephemeris time — ephem′eris time n. astron. time measured by the orbital movements of the earth, the moon, and the planets • Etymology: 1945–50 …   From formal English to slang

  • ephemeris time — noun Date: 1950 a uniform measure of time defined by the orbital motions of the planets …   New Collegiate Dictionary

  • ephemeris time — noun time on a scale defined by the orbital period rather than the axial rotation of the earth …   English new terms dictionary

  • Time from NPL — Map showing the location of the Anthorn VLF transmitter within Cumbria …   Wikipedia

Share the article and excerpts

Direct link
Do a right-click on the link above
and select “Copy Link”