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Greenwich Mean Time (GMT) is the mean solar time at the Royal Observatory in Greenwich, London. It is the timescale used in astronomy and navigation and most countries use it or a timezone offset for civil purposes. Astronomers refer to this timescale as UT1; when tabulating phenomena for civil use (e.g., lighting - up times, times of high tide) they call it GMT. Countries which do not use mean solar time for civil purposes use the scientific timescale Coordinated Universal Time (UTC), or a timezone offset from it, instead. UTC is not permitted to deviate from mean solar time by more than 0.9 seconds - it is brought into line by the addition of an occasional leap second. Coordinated Universal Time (with any necessary zone offset) is shown on radio - controlled clocks and given by analogue radio time signals. These are being phased out - digital radio time signals would be subject to a transmission delay of several seconds. In Britain, the legal time during the winter is Greenwich Mean Time. British Summer Time is one hour in advance. Greenwich Mean Time is also used by the European Union.

Because of Earth's uneven speed in its elliptical orbit and its axial tilt, noon (12:00:00) GMT is rarely the exact moment the sun crosses the Greenwich meridian and reaches its highest point in the sky there. This event may occur up to 16 minutes before or after noon GMT, a discrepancy calculated by the equation of time. Noon GMT is the annual average (i.e. "mean") moment of this event, which accounts for the word "mean" in "Greenwich Mean Time".

Originally, astronomers considered a GMT day to start at noon while for almost everyone else it started at midnight. To avoid confusion, the name Universal Time was introduced to denote GMT as counted from midnight. Astronomers preferred the old convention to simplify their observational data, so that each night was logged under a single calendar date. Today Universal Time usually refers to UTC or UT1.

The term "GMT" is especially used by bodies connected with the United Kingdom, such as the BBC World Service, the Royal Navy, the Met Office and others particularly in Arab countries, such as the Middle East Broadcasting Centre and OSN. It is a term commonly used in the United Kingdom and countries of the Commonwealth, including Australia, New Zealand, South Africa, India, Pakistan and Malaysia; and in many other countries of the eastern hemisphere.

History

As the United Kingdom grew into an advanced maritime nation, British mariners kept at least one chronometer on GMT to calculate their longitude from the Greenwich meridian, which was by convention considered to have longitude zero degrees, internationally adopted in the International Meridian Conference of 1884. Synchronisation of the chronometer on GMT did not affect shipboard time, which was still solar time. But this practice, combined with mariners from other nations drawing from Nevil Maskelyne's method of lunar distances based on observations at Greenwich, led to GMT being used worldwide as a standard time independent of location. Most time zones were based upon GMT, as an offset of a number of hours (and possibly a half-hour) "ahead of GMT" or "behind GMT".

Greenwich Mean Time was adopted across the island of Great Britain by the Railway Clearing House in 1847, and by almost all railway companies by the following year, from which the term "railway time" is derived. It was gradually adopted for other purposes, but a legal case in 1858 held "local mean time" to be the official time. On 14 May 1880, a letter signed by 'Clerk to Justices' appeared in 'The Times', stating that 'Greenwich time is now kept almost throughout England, but it appears that Greenwich time is not legal time. For example, our polling booths were opened, say, at 8 13 and closed at 4 13 PM.'This was changed later in 1880, when Greenwich Mean Time was legally adopted throughout the island of Great Britain. GMT was adopted on the Isle of Man in 1883, Jersey in 1898 and Guernsey in 1913. Ireland adopted GMT in 1916, supplanting Dublin Mean Time. Hourly time signals from Greenwich Observatory were first broadcast on 5 February 1924, rendering the time ball at the observatory redundant in the process.

The daily rotation of the Earth is irregular (see ΔT) but there is a long term slowing; therefore the atomic clocks constitute a much more stable timebase. On 1 January 1972, GMT was superseded as the international civil time standard by Coordinated Universal Time, maintained by an ensemble of atomic clocks around the world. Universal Time (UT), a term introduced in 1928, initially represented mean time at Greenwich determined in the traditional way to accord with the originally defined universal day; from 1 January 1956 (as decided by the IAU at Dublin, 1955, at the initiative of William Markowitz) this "raw" form of UT was re-labelled UT0 and effectively superseded by refined forms UT1 (UT0 equalised for the effects of polar wandering) and UT2 (UT1 further equalised for annual seasonal variations in earth rotation rate).

Indeed, even the Greenwich meridian itself is not quite what it used to be—defined by "the centre of the transit instrument at the Observatory at Greenwich". Although that instrument still survives in working order, it is no longer in use and now the meridian of origin of the world's longitude and time is not strictly defined in material form but from a statistical solution resulting from observations of all time-determination stations which the BIPM takes into account when co-ordinating the world's time signals. Nevertheless, the line in the old observatory's courtyard today differs no more than a few metres from that imaginary line which is now the prime meridian of the world.

— Howse, D. (1997). Greenwich time and the longitude. London: Philip Wilson.

Ambiguity in the definition of GMT

Historically GMT has been used with two different conventions for numbering hours. The long-standing astronomical convention dating from the work of Ptolemy, was to refer to noon as zero hours (see Julian day). This contrasted with the civil convention of referring to midnight as zero hours dating from the Romans. The latter convention was adopted on and after 1 January 1925 for astronomical purposes, resulting in a discontinuity of 12 hours, or half a day earlier. The instant that was designated 'December 31.5 GMT' in 1924 almanacs became 'January 1.0 GMT' in 1925 almanacs. The term Greenwich Mean Astronomical Time (GMAT) was introduced to unambiguously refer to the previous noon-based astronomical convention for GMT. The more specific terms UT and UTC do not share this ambiguity, always referring to midnight as zero hours.

GMT in legislation

United Kingdom

Legally, the civil time used in Britain is called still "Greenwich mean time" (without capitalisation), according to the Interpretation Act 1978, with an exception made for those periods when the Summer Time Act 1972 orders an hour's shift for daylight saving. The Interpretation Act 1978, section 9, provides that whenever an expression of time occurs in an Act, the time referred to shall (unless otherwise specifically stated) be held to be Greenwich mean time. Under subsection 23(3), the same rule applies to deeds and other instruments.

During the experiment of 1968-1971, when the British Isles did not revert to Greenwich Mean Time during the winter, the all-year British Summer Time was called British Standard Time (BST).

In Britain, UTC+0 is disseminated to the general public in winter and UTC+1 in summer.

BBC radio stations broadcast the "six pips" of the Greenwich Time Signal. It is named from its original generation at the Royal Greenwich Observatory, and is aligned to either Greenwich Mean Time or British Summer Time as appropriate for the time of year.

A coded radio signal is broadcast in the UK by Time from NPL.

As science is a precise discipline, various forms of atomic time have been devised to meet scientific needs. In scientific and technical fields, the use of the term "GMT" has been discouraged for decades.

Other countries

Most countries define their local time by reference to Greenwich Mean Time. Some examples are:

• Belgium: Decrees of 1946 and 1947 set legal time as one hour ahead of GMT.
• Ireland: Standard Time (Amendment) Act, 1971, section 1, and Interpretation Act 2005, part iv, section 18(i).
• Canada: Interpretation Act, R.S.C. 1985, c. I-21, section 35(1). This refers to 'standard time' for the several provinces, defining each in relation to 'Greenwich time', but does not use the expression 'Greenwich mean time'. Several provinces, such as Nova Scotia (Time Definition Act. R.S., c. 469, s. 1), have their own legislation which specifically mentions either "Greenwich Mean Time" or "Greenwich mean solar time".

Time zone

Those countries marked in dark blue on the map above use BST/Western European Summer Time and advance their clock one hour in summer. In the United Kingdom, this is British Summer Time (BST); in the Republic of Ireland it is called Irish Standard Time (IST)—officially changing to GMT in winter. Those countries marked in light blue keep their clocks on UTC/GMT/WET year round.

Discrepancies between legal GMT and geographical GMT

Since legal, political, social and economic criteria in addition to physical or geographical criteria are used in the drawing of time zones, actual time zones do not precisely adhere to meridian lines. The 'GMT' time zone, were it drawn by purely geographical terms, would consist of the area between meridians 7°30'W and 7°30'E. As a result, there are European locales that despite lying in an area with a 'physical' GMT time use another time zone (GMT+1 in particular); conversely, there are European areas that use GMT, even though their 'physical' time zone is GMT-1 (e.g., most of Portugal), or GMT−2 (the westernmost part of Iceland). Because the GMT time zone in Europe is 'shifted' to the west, Lowestoft in the United Kingdom at only 1°45'E is the easternmost settlement in Europe in which GMT is applied. Following is a list of the 'incongruencies':

Countries (or parts thereof) west of 22°30'W ("physical" GMT−2) that use GMT

• The westernmost part of Iceland, including the northwest peninsula and its main town of Ísafjörður, which is west of 22°30'W, uses GMT. Bjargtangar, Iceland is the westernmost point in which GMT is applied.

Countries (or parts thereof) west of 7°30'W ("physical" GMT−1) that use GMT

• Canary Islands (Spain)
• Most of Portugal, including Lisbon, Porto, Braga, Aveiro, and Coimbra. (Only the easternmost part, including cities such as Bragança and Guarda, lies east of 7°30'W.) Since the Treaty of Windsor in 1386 (the world's oldest diplomatic alliance), Portugal has maintained close ties to Britain, which possibly explains its choice of GMT. Madeira, even further to the west, also employs GMT. A more likely explanation is that during the mid-1970s, when Portugal was on Central European Time all year round, it did not begin to get light in Lisbon in winter until 08:30.
• Western part of Ireland, including the cities of Cork, Limerick, and Galway.
• Westernmost tip of Northern Ireland, including the county town of County Fermanagh, Enniskillen
• Extreme westerly portion of the Outer Hebrides, west of Scotland; for instance, Vatersay, an inhabited island and the westernmost settlement in Great Britain, lies at 7°54'W. If uninhabited islands or rocks are taken into account St Kilda, west of the Outer Hebrides, at 8°58'W, and Rockall, at 13°41'W, should be included.
• Westernmost island of the Faroe Islands (autonomous region of the Danish Kingdom), Mykines
• Iceland, including Reykjavík
• Northeastern part of Greenland, including Danmarkshavn

Countries (mostly) between meridians 7°30'W and 7°30'E ("physical" GMT) that use GMT+1

• Spain (except for the Canary Islands, which use GMT). Parts of Galicia lie west of 7°30'W ('physical' GMT−1), whereas there is no Spanish territory east of 7°30'E ('physical' GMT+1). Spain's time is the direct result of Franco's Presidential Order (published in Boletín Oficial del Estado of 8 March 1940) abandoning Greenwich Mean Time and advancing clocks one hour effective 23:00 16 March 1940. This is an excellent example of political criteria used in the drawing of time zones: the time change was passed "in consideration of the convenience from the national time marching in step according to that of other European countries". The Presidential Order (most likely enacted to be in synchrony with Germany and Italy, with which the Franco regime was unofficially allied) included in its 5th article a provision for its future phase out, which never took place. Due to this political decision Spain is two hours ahead of its local mean time during the summer, one hour ahead in winter, which possibly explains the notoriously late schedule for which the country is known. In Portugal, which is a mere one hour behind Spain, the timetable is quite different.
• Most of France, including the cities of Paris, Marseilles and Lyon. Only small parts of Alsace, Lorraine and Provence are east of 7°30'E ("physical" GMT+1).
• Monaco
• Andorra
• Belgium
• Netherlands
• Luxembourg

See also

• Greenwich Time Signal
• 24-hour watch—24-hour wristwatch
• Radio clock
• Marine chronometer—synchronised with GMT, and used by ships to calculate their longitude
• Sandringham Time
• Swatch Internet Time—alternative, decimal measure of time
• Western European Summer Time

Notes

1. U S Naval Observatory Astronomical Applications Department (11 August 2015). "The Equation ofTime". Retrieved 6 November 2016. UT1 is determined by astronomical observations, and it can be considered the modern equivalent of Greenwich Mean Time, that is, mean solar time at longitude zero.
2. Seidelmann, P Kenneth; Guinot, B; Doggett, L E (2006). "'Time', in P Kenneth Seidelmann (ed.), Explanatory Supplement to the Astronomical Almanac". Sausalito, CA. pp. 53–54. ISBN 1-891389-45-9. Retrieved 6 November 2016.
3. National Physical Laboratory (31 March 2015). "At what time should clocks go forward or back for summer time (FAQ - Time)". Retrieved 6 November 2016. The time at which summer time begins and ends is given in the relevant EU Directive and UK Statutory Instrument as 1 a.m. Greenwich Mean Time (GMT) ... All time signals are based on Coordinated Universal Time (UTC), which can be almost one second ahead of, or behind, GMT so there is a brief period in the UK when the directive is not being strictly followed.
4. ^ McCarthy & Seidelmann 2009, p. 17.
5. Astronomical Almanac Online 2015, Glossary s.v. "Universal Time"
6. Howse 1997, p. 114.
7. CLERK TO JUSTICES. "Time, Actual And Legal". Times, London, England, 14 May 1880: 10. The Times Digital Archive. Web. 18 Aug. 2015.
8. Bartky, Ian R. (2007). One Time Fits All: The Campaigns for Global Uniformity. Stanford University Press. p. 134. ISBN 0804756422. Retrieved 18 August 2015.
9. ^ Myers (2007).
10. UT1 as explained on IERS page.
11. Astronomical Supplement to the Astronomical Almanac. University Science Books. 1992. p. 76. ISBN 0-935702-68-7.
12. Howse 1997, p. 157.
13. Seidelmann, P Kenneth. (2013). "Introduction to Positional Astronomy" in Sean E Urban and P Kenneth Seidelmann, eds. Explanatory Supplement to the Astronomical Almanac 3rd ed. Mill Valley, CA: University Science Books p. 14. "In the past the term 'Greenwich Mean Time' (GMT) has been used for UTC and it remains the basis of the civil time for the United Kingdom, and as such is related to UTC. However, in navigational terminology, GMT means Universal Time. For precise purposes it is recommended that the term 'GMT' not be used, since it is ambiguous."
14. McCarthy and Seidelmann (p. 17) devote most of a page explaining why "the use of the term 'Greenwich Mean Time' or its abbreviation 'GMT' remains a source of confusion today." They point out several times when respected authorities have stopped using the name GMT or recommended that the name GMT should no longer be used: the IAU in 1928, the 1939 American Ephemeris, astronomical almanacs after 1960, and another recommendation from the IAU in 1976.
15. ^ Dumortier, Hannelore, & Loncke (n.d.).
16. Seago & Seidelmann (c. 2001).
17. Standard Time Act, 1968.
18. "BOE Orden sobre adelanto de la hora legal en 60 minutos". Retrieved 2 December 2008.
19. "B.O.E. #68 03/08/1940 p.1675". Retrieved 2 December 2008.
20. ^ "B.O.E. #68 03/08/1940 p.1676". Retrieved 2 December 2008.
21. "Hábitos y horarios españoles". Retrieved 27 November 2008.

References

• Astronomical Almanac Online. (2015). United States Naval Observatory and Her Majesty's Nautical Almanac Office.
• Dumortier, J, Hannelore, D, & Loncke, M. (n.d.). "Legal Aspects of Trusted Time services in Europe". AMANO. Retrieved 8 July 2009.
• Guinot, Bernard (August 2011). "Solar time, legal time, time in use". Metrologica 48 (4): S181–185. Bibcode:2011Metro..48S.181G. doi:10.1088/0026-1394/48/4/S08.
• Hilton, James L and McCarthy, Dennis D.. (2013). "Precession, Nutation, Polar Motion, and Earth Rotation." In Sean Urban and P. Kenneth Seidelmann (Eds.), Explanatory Supplement to the Astronomical Almanac 3rd ed. Mill Valley CA: University Science Books.
• Howse, D. (1997). Greenwich time and the longitude. London: Philip Wilson.
• Interpretation Act, R.S.C. 1985, c. I-21. (2005). CanLII. (Canadian statute).
• Interpretation Act 1978. UK Law Statute Database. (UK statute).
• Interpretation Act 2005. British and Irish Legal Information Institute. (Irish statute).
• McCarthy, D., and Seidelmann, P. K. (2009). TIME—From Earth Rotation to Atomic Physics. Weinheim: Wiley-VCH.
• Myers, J. (2007). History of legal time in Britain. Retrieved 4 January 2008.
• Seago, J.H., & Seidelmann, P. K. (c. 2001). National Legal Requirements for Coordinating with Universal Time. Steve Allen of University of California Observatories. Retrieved 8 July 2009.
• "Six pip salute". BBC News. Retrieved 9 July 2009.
• Standard Time Act, 1968. Irish Statute Book. Office of the Attorney General. (Irish statute).
• Standard Time (Amendment) Act, 1971. British and Irish Legal Information Institute. (Irish statute).

External links

• Greenwich Mean Time.
• Interactive World Clock Map in Flash.
• International Earth Rotation and Reference Systems Service.
• Royal Observatory, Greenwich.
• The original BBC World Service GMT time signal in mp3 format.
• Rodgers, Lucy (20 October 2009). "At the centre of time". BBC News. Retrieved 20 October 2009.

v t e Time measurement and standards
Chronometry Orders of magnitude Metrology
International standards	Coordinated Universal Time offset UT ΔT DUT1 International Earth Rotation and Reference Systems Service ISO 31-1 ISO 8601 International Atomic Time 12-hour clock 24-hour clock Barycentric Coordinate Time Barycentric Dynamical Time Civil time Daylight saving time Geocentric Coordinate Time International Date Line IERS Reference Meridian Leap second Solar time Terrestrial Time Time zone 180th meridian
Obsolete standards	Ephemeris time Greenwich Mean Time Prime meridian
Time in physics	Absolute space and time Spacetime Chronon Continuous signal Coordinate time Cosmological decade Discrete time and continuous time Proper time Theory of relativity Time dilation Gravitational time dilation Time domain Time-translation symmetry T-symmetry
Horology	Clock Astrarium Atomic clock Complication History of timekeeping devices Hourglass Marine chronometer Marine sandglass Radio clock Watch stopwatch Water clock Sundial Dialing scales Equation of time History of sundials Sundial markup schema
Calendar	Gregorian Hebrew Hindu Holocene Islamic (lunar Hijri) Julian Solar Hijri Astronomical Dominical letter Epact Equinox Intercalation Julian day Leap year Lunar Lunisolar Solar Solstice Tropical year Weekday determination Weekday names
Archaeology and geology	Chronological dating Geologic time scale International Commission on Stratigraphy
Astronomical chronology	Galactic year Nuclear timescale Precession Sidereal time
Other units of time	Instant Flick Shake Jiffy Second Minute Moment Hour Day Week Fortnight Month Year Olympiad Lustrum Decade Century Saeculum Millennium
Related topics	Chronology Duration music Mental chronometry Decimal time Metric time System time Time metrology Time value of money Timekeeper

• Use dmy dates from July 2012
• Geography of Greenwich
• Time zones
• Time in the United Kingdom
• 1884 introductions