UT is defined by a mathematical formula relating UT to sidereal time. It is thus determined from observations of the diurnal motions of stars. It is not a uniform timescale, however, due to variations in the Earth's rotation. The timescale determined directly from stellar observations is dependent on the place of observation, and is designated UT0. The timescale independent of location is obtained by correcting UT0 for the variation in the observer's meridian that arises from the irregular varying motion of the Earth's geographical poles; it is designated UT1. This is the timescale used by astronomers. It is counted from 0 hours at midnight, and the unit is the mean solar day.
Coordinated universal time (UTC) is based on International Atomic Time (TAI). Since Jan. 1 1972 the time given by broadcast time signals has been UTC. UTC differs from TAI by an integral number of seconds. UTC is kept within 0.90 seconds of UT1 by the insertion (or deletion) of exactly one second when necessary, usually at the end of December or June; these step adjustments are termed leap seconds. An approximation (DUT1) to the value of UT1 minus UTC is transmitted in code on broadcast time signals. TAI and UTC are recommended for the precise dating of observations. See also dynamical time.
