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Basics

TAI (International Atomic Time)

tai

Definition

TAI (Temps Atomique International, or International Atomic Time) is a timescale produced by statistically combining data from approximately 450 atomic clocks maintained by over 80 national metrology laboratories. The International Bureau of Weights and Measures (BIPM) in Paris performs the computation. TAI is a continuous timescale with no leap seconds, running from its epoch of 1 January 1958 00:00:00 (UT2).

Relationship to UTC

UTC is derived from TAI by applying leap-second adjustments. As of 2026, UTC = TAI - 37 seconds. This offset is the sum of 27 leap seconds inserted since 1972 and the initial 10-second difference established when UTC was introduced. In a 2022 resolution, the General Conference on Weights and Measures (CGPM) decided that the maximum permitted difference between UT1 and UTC will be widened by 2035. The new limit and its implementation date were still undecided as of September 2026, but once the limit is widened, leap second insertions will effectively end and the TAI-UTC difference in force at that time will be retained.

How It Is Computed

TAI is calculated retrospectively. Data from participating clocks are collected over roughly one month, then processed statistically and published in a monthly bulletin called Circular T. No real-time TAI signal is broadcast; instead, each laboratory maintains its own real-time realization of UTC, called UTC(k), and that is what serves as a practical time reference. The real-time counterpart on the TAI side is TAI(k), which currently equals UTC(k) plus 37 seconds. In Japan, NICT maintains UTC(NICT) as the local realization of the standard.

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