International Atomic Time

Operation

TAI is a weighted average of the time kept by over 450 atomic clocks in over 80 national laboratories worldwide.{{cite book |access-date = 16 June 2022 |archive-url=https://web.archive.org/web/20210814134522/https://webtai.bipm.org/ftp/pub/tai/annual-reports/bipm-annual-report/annual_report_2020.pdf |archive-date=14 August 2021 |url-status=live}} The majority of the clocks involved are caesium clocks; the International System of Units (SI) definition of the second is based on caesium. The clocks are compared using GPS signals and two-way satellite time and frequency transfer. Due to the signal averaging TAI is an order of magnitude more stable than its best constituent clock.

The participating institutions each broadcast, in real time, a frequency signal with timecodes, which is their estimate of TAI. Time codes are usually published in the form of UTC, which differs from TAI by a well-known integer number of seconds. These time scales are denoted in the form UTC(NPL) in the UTC form, where NPL here identifies the National Physical Laboratory, UK. The TAI form may be denoted TAI(NPL). The latter is not to be confused with TA(NPL), which denotes an independent atomic time scale, not synchronised to TAI or to anything else.

The clocks at different institutions are regularly compared against each other. The International Bureau of Weights and Measures (BIPM, France) combines these measurements to retrospectively calculate the weighted average that forms the most stable time scale possible. This combined time scale is published monthly in "Circular T" and is the canonical TAI. This time scale is expressed in the form of tables of differences UTC− UTC(k) (equal to TAI− TAI(k)) for each participating institution k. The same circular also gives tables of TAI− TA(k), for the various unsynchronised atomic time scales.

Errors in publication may be corrected by issuing a revision of the faulty Circular T or by errata in a subsequent Circular T. Aside from this, once published in Circular T, the TAI scale is not revised. In hindsight, it is possible to discover errors in TAI and to make better estimates of the true proper time scale. Since the published circulars are definitive, better estimates do not create another version of TAI; it is instead considered to be creating a better realisation of Terrestrial Time (TT).

History

Early atomic time scales consisted of quartz clocks with frequencies calibrated by a single atomic clock; the atomic clocks were not operated continuously. Atomic timekeeping services started experimentally in 1955, using the first caesium atomic clock at the National Physical Laboratory, UK (NPL). It was used as a basis for calibrating the quartz clocks at the Royal Greenwich Observatory and to establish a time scale, called Greenwich Atomic (GA). The United States Naval Observatory began the A.1 scale on 13 September 1956, using an Atomichron commercial atomic clock, followed by the NBS-A scale at the National Bureau of Standards, Boulder, Colorado on 9 October 1957.

The International Time Bureau (BIH) began a time scale, Tm or AM, in July 1955, using both local caesium clocks and comparisons to distant clocks using the phase of VLF radio signals. The BIH scale, A.1, and NBS-A were defined by an epoch at the beginning of 1958 The procedures used by the BIH evolved, and the name for the time scale changed: A3 in 1964 and TA(BIH) in 1969.

The SI second was defined in terms of the caesium atom in 1967. From 1971 to 1975, the General Conference on Weights and Measures and the International Committee for Weights and Measures made a series of decisions that designated the BIPM time scale International Atomic Time (TAI).

In the 1970s, it became clear that the clocks participating in TAI were ticking at different rates due to gravitational time dilation, and the combined TAI scale, therefore, corresponded to an average of the altitudes of the various clocks. Starting from the Julian Date 2443144.5 (1 January 1977 00:00:00 TAI), corrections were applied to the output of all participating clocks, so that TAI would correspond to proper time at the geoid (mean sea level). Because the clocks were, on average, well above sea level, this meant that TAI slowed by about one part in a trillion. The former uncorrected time scale continues to be published under the name EAL (Échelle Atomique Libre, meaning Free Atomic Scale).

The instant that the gravitational correction started to be applied serves as the epoch for Barycentric Coordinate Time (TCB), Geocentric Coordinate Time (TCG), and Terrestrial Time (TT), which represent three fundamental time scales in the Solar System. All three of these time scales were defined to read JD 2443144.5003725 (1 January 1977 00:00:32.184) exactly at that instant. TAI was henceforth a realisation of TT, with the equation TT(TAI) = TAI + 32.184 s.

The continued existence of TAI was questioned in a 2007 letter from the BIPM to the ITU-R, which stated, "In the case of a redefinition of UTC without leap seconds, the CCTF would consider discussing the possibility of suppressing TAI, as it would remain parallel to the continuous UTC."{{cite web |access-date=24 September 2018 |archive-url=https://web.archive.org/web/20120316100907/http://www.bipm.org/cc/CCTF/Allowed/18/CCTF_09-27_note_on_UTC-ITU-R.pdf |archive-date=16 March 2012 |url-status=dead

Relation to UTC

Contrary to TAI, UTC is a discontinuous time scale. It is occasionally adjusted by leap seconds. Between these adjustments, it is composed of segments that are mapped to atomic time by a constant offset. From its beginning in 1961 through December 1971, the adjustments were made regularly in fractional leap seconds so that UTC approximated UT2. Afterwards, these adjustments were made only in whole seconds to approximate UT1. This was a compromise arrangement in order to enable a publicly broadcast time scale. The less frequent whole-second adjustments meant that the time scale would be more stable and easier to synchronize internationally. The fact that it continues to approximate UT1 means that tasks, such as navigation, which require a source of Universal Time continue to be well served by the public broadcast of UTC.

Notes

References

• {{cite web |archive-url=https://web.archive.org/web/20250305025122/https://maia.usno.navy.mil/ser7/tai-utc.dat |url-status=live |archive-date=5 March 2025 |access-date=13 May 2025
• {{cite web |access-date=24 January 2020 |archive-url=https://web.archive.org/web/20110110113226/http://www.bipm.org/en/scientific/tai/tai.html |archive-date=10 January 2011 |url-status=dead

Footnotes

Bibliography

• {{ cite book | archive-url=https://web.archive.org/web/20220801225534/https://www.google.com/books/edition/Polar_Motion/pFDwAAAAMAAJ?hl=en | archive-date=1 August 2022 | url-status=live
• {{Cite book |author-link=Dennis D. McCarthy |access-date=12 June 2021 |archive-date=3 February 2021 |archive-url=https://web.archive.org/web/20210203233222/https://books.google.com/books?id=7NdrK4e77CIC |url-status=live

References

1. Temps atomique 1975{{elucidate. (April 2020)
2. (1986). "Is the International Atomic Time TAI a coordinate time or a proper time?". Celestial Mechanics.
3. Bizouard, Christian. (6 January 2026). "Bulletin C 71". [[IERS]].
4. Bizouard, Christian. (6 July 2016). "Bulletin C 52". [[IERS]].
5. (2022-11-18). "Do not adjust your clock: scientists call time on the leap second". The Guardian.
6. (12 July 2021). "Explanatory Supplement of BIPM Circular T". [[International Bureau of Weights and Measures]].
7. "Circular T". [[International Bureau of Weights and Measures]].
8. "The epoch of TAI is 1961-01-01T20:00:00 UT2". UCO/Lick Observatory.
9. (March 1990). "Relativistic time scales in the solar system". [[Celestial Mechanics and Dynamical Astronomy]].