What is Time?
Time is the way we measure change and sequence events — from the ticking of atoms in laboratories to the daily rising of the Sun. This page explains how modern timekeeping works, why hours, minutes and seconds exist, and what keeps our clocks honest.
Origins of timekeeping
Early humans used the Sun and Moon to mark days and months. Sundials and water clocks (clepsydra) tracked daytime and night-time hours. Mechanical escapement clocks in medieval Europe allowed continuous counting of hours — and led to the daily schedules of modern life.
Why we still correct time (leap seconds)
The Earth's rotation slows slightly due to tidal friction, so astronomers sometimes insert leap seconds into UTC to keep civil time aligned with the mean solar day. Leap seconds are announced by the International Earth Rotation and Reference Systems Service (IERS). They are rare and unpredictable.
Last leap second added: 31 December 2016 (UTC). Because leap seconds are scheduled irregularly, there is no permanent countdown until IERS announces one.
How we handle it here
- If a leap second is announced, clocks are adjusted on the announced UTC timestamp.
- Atomic clocks continue to measure SI seconds reliably — GPS and international time services manage the correction.