can be used to measure the passage of one
hour of time. It also concretely represents the present as being between the past and the future. Methods of temporal measurement, or
chronometry, generally take two forms. The first is a
calendar, a mathematical tool for organising intervals of time on Earth, consulted for periods longer than a day. The second is a
clock, a physical mechanism that indicates the passage of time, consulted for periods less than a day. The combined measurement marks a specific moment in time from a reference point, or
epoch. Time is one of the seven fundamental
physical quantities in both the
International System of Units (SI) and
International System of Quantities. The SI base
unit of time is the
second, which is defined by measuring the
electronic transition frequency of
caesium atoms.
History of the calendar Artifacts from the
Paleolithic suggest that the moon was being used to reckon time by at least 6,000 years ago.
Lunar calendars were among the first to appear, with years of either 12 or 13
lunar months (either 354 or 384 days). Without
intercalation to add days or months to some years, seasons quickly drift in a calendar based solely on twelve lunar months.
Lunisolar calendars have a thirteenth month added to some years to make up for the difference between a full year (now known to be about 365.24 days) and a year of just twelve lunar months. The numbers twelve and thirteen came to feature prominently in many cultures, at least partly due to this relationship of months to years. Other early forms of calendars originated in
Mesoamerica, particularly in ancient Mayan civilization, in which they developed the
Maya calendar, consisting of multiple interrelated calendars. These calendars were religiously and astronomically based; the
Haab' calendar has 18 months in a year and 20 days in a month, plus five
epagomenal days at the end of the year. In conjunction, the Maya also used a 260-day sacred calendar called the
Tzolk'in. The reforms of
Julius Caesar in 45 BC put the
Roman world on a
solar calendar. This
Julian calendar was faulty in that its intercalation still allowed the astronomical
solstices and
equinoxes to advance against it by about 11 minutes per year.
Pope Gregory XIII introduced a correction in 1582; the
Gregorian calendar was only slowly adopted by different nations over a period of centuries, but it is now by far the most commonly used calendar around the world. During the
French Revolution, a new clock and calendar were invented as part of the
dechristianization of France and to create a more rational system in order to replace the Gregorian calendar. The
French Republican Calendar's days consisted of ten hours of a hundred minutes of a hundred seconds, which marked a deviation from the base 12 (
duodecimal) system used in many other devices by many cultures. The system was abolished in 1806.
History of other devices in Canberra A large variety of
devices have been invented to measure time. The study of these devices is called
horology. They can be driven by a variety of means, including gravity, springs, and various forms of electrical power, and regulated by a variety of means. A
sundial is any device that uses the direction of sunlight to cast shadows from a
gnomon onto a set of markings calibrated to indicate the
local time, usually to the hour. The idea to separate the day into smaller parts is credited to Egyptians because of their sundials, which operated on a duodecimal system. The importance of the number 12 is due to the number of lunar cycles in a year and the number of stars used to count the passage of night.
Obelisks made as a gnomon were built as early as . An Egyptian device that dates to , similar in shape to a bent
T-square, also measured the passage of time from the shadow cast by its crossbar on a nonlinear rule. The T was oriented eastward in the mornings. At noon, the device was turned around so that it could cast its shadow in the evening direction. Alarm clocks reportedly first appeared in ancient Greece with a water clock made by
Plato that would set off a whistle. The hydraulic alarm worked by gradually filling a series of vessels with water. After some time, the water emptied out of a
siphon. Inventor
Ctesibius revised Plato's design; the water clock uses a float as the power drive system and uses a sundial to correct the water flow rate. In medieval philosophical writings, the atom was a unit of time referred to as the smallest possible division of time. The earliest known occurrence in English is in
Byrhtferth's
Enchiridion (a science text) of 1010–1012, where it was defined as 1/564 of a
momentum (1 minutes), and thus equal to 15/94 of a second. It was used in the
computus, the process of calculating the date of Easter. The most precise timekeeping device of the
ancient world was the
water clock, or
clepsydra, one of which was found in the tomb of Egyptian pharaoh
Amenhotep I. They could be used to measure the hours even at night but required manual upkeep to replenish the flow of water. The
ancient Greeks and the people from
Chaldea (southeastern Mesopotamia) regularly maintained timekeeping records as an essential part of their astronomical observations. Arab inventors and engineers, in particular, made improvements on the use of water clocks up to the Middle Ages. In the 11th century,
Chinese inventors and
engineers invented the first mechanical clocks driven by an
escapement mechanism. , 2007 Incense sticks and candles were, and are, commonly used to measure time in temples and churches across the globe. Water clocks, and, later, mechanical clocks, were used to mark the events of the abbeys and monasteries of the Middle Ages. The passage of the hours at sea can also be marked by
bell. The hours were marked by bells in abbeys as well as at sea.
Richard of Wallingford (1292–1336), abbot of St. Alban's abbey, famously built a mechanical clock as an astronomical
orrery about 1330. The
hourglass uses the flow of sand to measure the flow of time. They were also used in navigation.
Ferdinand Magellan used 18 glasses on each ship for his circumnavigation of the globe (1522). The English word
clock probably comes from the Middle Dutch word
klocke which, in turn, derives from the medieval Latin word
clocca, which ultimately derives from Celtic and is cognate with French, Latin, and German words that mean
bell. Great advances in accurate time-keeping were made by
Galileo Galilei and especially
Christiaan Huygens with the invention of pendulum-driven clocks along with the invention of the minute hand by Jost Burgi. There is also a clock that was designed to keep time for 10,000 years called the
Clock of the Long Now. Alarm clock devices were later mechanized.
Levi Hutchins alarm clock has been credited as the first American alarm clock, though it can only ring at 4 a.m.
Antoine Redier was also credited as the first person to patent an adjustable mechanical alarm clock in 1847. Digital forms of alarm clocks became more accessible through digitization and integration with other technologies, such as
smartphones. s, such as this one unveiled in 2004, are expected to greatly improve
GPS location. The most accurate timekeeping devices are
atomic clocks, which are accurate to seconds in many millions of years, and are used to calibrate other clocks and timekeeping instruments. Atomic clocks use the frequency of
electronic transitions in certain atoms to measure the second. One of the atoms used is
caesium; most modern atomic clocks probe caesium with microwaves to determine the frequency of these electron vibrations. Since 1967, the International System of Measurements bases its unit of time, the second, on the properties of caesium atoms.
SI defines the second as 9,192,631,770 cycles of the radiation that corresponds to the transition between two electron spin energy levels of the ground state of the 133Cs atom. A portable timekeeper that meets certain precision standards is called a
chronometer. Initially, the term was used to refer to the
marine chronometer, a timepiece used to determine
longitude by means of
celestial navigation, a precision first achieved by
John Harrison. More recently, the term has also been applied to the
chronometer watch, a watch that meets precision standards set by the Swiss agency
COSC. In modern times, the
Global Positioning System in coordination with the
Network Time Protocol can be used to synchronize timekeeping systems across the globe. , the smallest time interval uncertainty in direct measurements is on the order of 12
attoseconds (1.2 × 10−17 seconds), about 3.7 × 1026
Planck times. The time measured was the delay caused by out-of-sync electron waves'
interference patterns.
Units The second (s) is the
SI base unit. A
minute (min) is 60 seconds in length (or, rarely, 59 or 61 seconds when leap seconds are employed), and an
hour is 60 minutes or 3600 seconds in length. A day is usually 24 hours or 86,400 seconds in length; however, the duration of a calendar day can vary due to
daylight saving time and
leap seconds.
Standards A time standard is a specification for measuring time: assigning a number or
calendar date to an
instant (point in time), quantifying the duration of a time interval, and establishing a
chronology (ordering of events). In modern times, several time specifications have been officially recognized as standards, where formerly they were matters of custom and practice. The invention in 1955 of the caesium
atomic clock has led to the replacement of older and purely astronomical time standards such as
sidereal time and
ephemeris time, for most practical purposes, by newer time standards based wholly or partly on atomic time using the SI second.
International Atomic Time (TAI) is the primary international time standard from which other time standards are calculated.
Universal Time (UT1) is mean solar time at 0° longitude, computed from astronomical observations. It varies from TAI because of the irregularities in Earth's rotation.
Coordinated Universal Time (UTC) is an atomic time scale designed to approximate Universal Time. UTC differs from TAI by an integral number of seconds. UTC is kept within 0.9 second of UT1 by the introduction of one-second steps to UTC, the
leap second. The
Global Positioning System broadcasts a very precise time signal based on UTC time. The surface of the Earth is split into a number of
time zones. Standard time or
civil time in a time zone deviates a fixed, round amount, usually a whole number of hours, from some form of Universal Time, usually UTC. Most time zones are exactly one hour apart, and by convention compute their local time as an offset from UTC. For example, time zones at sea are based on UTC. In many locations (but not at sea) these offsets vary twice yearly due to
daylight saving time transitions. Some other time standards are used mainly for scientific work.
Terrestrial Time is a theoretical ideal scale realized by TAI.
Geocentric Coordinate Time and
Barycentric Coordinate Time are scales defined as
coordinate times in the context of the general theory of relativity, with TCG applying to Earth's center and TCB to the solar system's
barycenter.
Barycentric Dynamical Time is an older relativistic scale related to TCB that is still in use. == Philosophy ==