A prime meridian is a meridian, i.e. a line of longitude, at which longitude is defined to be 0°. A prime meridian and its opposite in a 360°-system, the 180th meridian (at 180° longitude), form a great circle.
This great circle divides the sphere, e.g. the Earth, into two hemispheres. If one uses directions of East and West from a defined prime meridian, then they can be called Eastern Hemisphere and Western Hemisphere.
A prime meridian is ultimately arbitrary, unlike an equator, which is determined by the axis of rotation—and various conventions have been used or advocated in different regions and throughout history.
The notion of longitude was developed by the Greek Eratosthenes (c. 276 BC – c. 195 BC) in Alexandria and Hipparchus (c. 190 BC – c. 120 BC) in Rhodes and applied to a large number of cities by the geographer Strabo (64/63 BC – c. 24 AD). But it was Ptolemy (c. AD 90 – c. AD 168) who first used a consistent meridian for a world map in his Geographia.
Ptolemy used as his basis the "Fortunate Isles", a group of islands in the Atlantic which are usually associated with the Canary Islands (13° to 18°W), although his maps correspond more closely to the Cape Verde islands (22° to 25° W). The main point is to be comfortably west of the western tip of Africa (17.5° W) as negative numbers were not yet in use. His prime meridian corresponds to 18° 40' west of Winchester (about 20°W) today. At this time the chief method of determining longitude was by using the reported times of lunar eclipses in different countries.
Ptolemy’s Geographia was first printed with maps at Bologna in 1477 and many early globes in the sixteenth century followed his lead. But there was still a hope that a "natural" basis for a prime meridian existed. Christopher Columbus reported (1493) that the compass pointed due north somewhere in mid-Atlantic and this fact was used in the important Tordesillas Treaty of 1494 which settled the territorial dispute between Spain and Portugal over newly discovered lands. The Tordesillas line was eventually settled at 370 leagues west of Cape Verde. This is shown in Diogo Ribeiro's 1529 map. São Miguel Island (25.5°W) in the Azores was still used for the same reason as late as 1594 by Christopher Saxton, although by this time it had been shown that the zero deviation line did not follow a line of longitude.
In 1541, Mercator produced his famous forty-one centimetre terrestrial globe and drew his prime meridian precisely through Fuertaventura (14°1'W) in the Canaries. His later maps used the Azores, following the magnetic hypothesis. But by the time that Ortelius produced the first modern atlas in 1570, other islands such as Cape Verde were coming into use. In his atlas longitudes were counted from 0° to 360°, not 180°W to 180°E as is common today. This practice was followed by navigators well into the eighteenth century. In 1634, Cardinal Richelieu used the westernmost island of the Canaries, Ferro, 19° 55' west of Paris, as the choice of meridian. Unfortunately, the geographer Delisle decided to round this off to 20°, so that it simply became the meridian of Paris disguised.
In the early eighteenth century the battle was on to improve the determination of longitude at sea, leading to the development of the chronometer by John Harrison. But it was the development of accurate star charts principally by the first British Astronomer Royal, John Flamsteed between 1680 and 1719 and disseminated by his successor, Edmund Halley that enabled navigators to use the lunar method of determining longitude more accurately using the octant developed by Thomas Godfrey and John Hadley. Between 1765 and 1811, Nevil Maskelyne published 49 issues of the Nautical Almanac based on the meridian of the Royal Observatory, Greenwich. "Maskelyne's tables not only made the lunar method practicable, they also made the Greenwich meridian the universal reference point. Even the French translations of the Nautical Almanac retained Maskelyne's calculations from Greenwich—in spite of the fact that every other table in the Connaissance des Temps considered the Paris meridian as the prime." 
In 1884, at the International Meridian Conference held in Washington, D.C., 22 countries voted to adopt the Greenwich meridian as the prime meridian of the world. The French argued for a neutral line, mentioning the Azores and the Bering Strait but eventually abstained and continued to use the Paris meridian until 1911.
List of other prime meridians on Earth
|Locality||GPS longitude||Meridian name||Comment|
|Bering Strait||168°30′ W||
|Washington, D.C.||77°03′56.07″ W (1897) or 77°04′02.24″ W (NAD 27) or 77°04′01.16″ W (NAD 83)||New Naval Observatory Meridian|
|Washington, D.C.||77°02′48.0″ W, 77°03′02.3″, 77°03′06.119″ W or 77°03′06.276″ W (both presumably NAD 27). If NAD27, the latter would be 77°03′05.194″ W (NAD 83)||Old Naval Observatory Meridian|
|Washington, D.C.||77°02′11.56258″ W (NAD 83), 77°02′11.55880″ W (NAD 83), 77°02′11.57375″ W (NAD 83)||White House Meridian|
|Washington, D.C.||77°00′32.6″ W (NAD 83)||Capitol meridian|
|Philadelphia||75° 10′ 12″ W|
|Rio de Janeiro||43° 10′ 19″ W|||
|Fortunate Isles / Azores||~ 25° 40′ 32″ W||Used until the Middle Ages, proposed as one possible neutral meridian by Pierre Janssen at the International Meridian Conference|
|El Hierro (Ferro),
|18° 03′ W,
later redefined as
17° 39′ 46″? W
|Lisbon||9° 07′ 54.862″ W|
|Madrid||3° 41′ 16.58″ W|
|Greenwich||0° 00′ 05.3101″ W||Greenwich meridian||Airy Meridian|
|Greenwich||0° 00′ 05.33″ W||United Kingdom Ordnance Survey Zero Meridian||Bradley Meridian|
|Greenwich||0° 00′ 00.00″ W||IERS Reference Meridian|
|Paris||2° 20′ 14.025″ E||Paris meridian|
|Brussels||4° 22′ 4.71″ E|
|Antwerp||4° 24′ E||Antwerp Meridian||used by Mercator|
|Bern||7° 26′ 22.5″ E|
|Oslo (Kristiania)||10° 43′ 22.5″ E|
|Florence||11°15′ E||Florence Meridian||used in the Peters projection, antipode of a line running through the Bering Strait|
|Rome||12° 27′ 08.4″ E||meridian of Monte Mario|
|Copenhagen||12° 34′ 32.25″ E||Rundetårn|
|Naples||14° 15′ E|||
|Stockholm||18° 03′ 29.8″ E||at the Stockholm Observatory|
|Warsaw||21° 00′ 42″ E||Warsaw Meridian|
|Oradea||21° 55′ 16″ E|
|Alexandria||29° 53′ E|||
|Saint Petersburg||30° 19′ 42.09″ E||Pulkovo Meridian|
|Great Pyramid of Giza||31° 08′ 03.69″ E||1884 |
|Jerusalem||35° 13′ 47.1″ E||for the small dome of the Church of the Holy Sepulchre|
|Mecca||39° 49′ 34″ E||see Mecca Time Approximately 59° east of Greenwich |
|Ujjain||75° 47′ E||Used from 4th century CE Indian astronomy and calendars.|
|Kyoto||135° 74′ E||Used in 18th and 19th (officially 1779-1871) century Japanese maps. Exact place unknown, but in "Kairekisyo" in Nishigekkoutyou-town in Kyoto, then the capital.|
|~ 180||Opposite of Greenwich, proposed 13 Oct 1884 on the International Meridian Conference by Sandford Fleming |
International prime meridian
In October 1884 the Greenwich Meridian was selected by delegates (forty-one delegates representing twenty-five nations) to the International Meridian Conference held in Washington, D.C., United States to be the common zero of longitude and standard of time reckoning throughout the world.
Prime meridian at Greenwich
The position of the Greenwich Meridian has been defined by the location of the Airy transit circle ever since the first observation was taken with it by Sir George Airy in 1851. Prior to that, it was defined by a succession of earlier transit instruments, the first of which was acquired by the second Astronomer Royal, Edmond Halley in 1721. It was set up in the extreme north-west corner of the Observatory between Flamsteed House and the Western Summer House. This spot, now subsumed into Flamsteed House, is roughly 43 metres to the west of the Airy Transit Circle, a distance equivalent to roughly 0.15 seconds of time. It was Airy's transit circle that was adopted in principle (with French delegates, who pressed for adoption of the Paris meridian abstaining) as the Prime Meridian of the world in 1884.
All of these Greenwich meridians were located via an astronomic observation from the surface of the Earth, oriented via a plumb line along the direction of gravity at the surface. This astronomic Greenwich meridian was disseminated around the world, first via the lunar distance method, then by chronometers carried on ships, then via telegraph lines carried by submarine communications cables, then via radio time signals. One remote longitude ultimately based on the Greenwich meridian using these methods was that of the North American Datum 1927 or NAD27, an ellipsoid whose surface best matches mean sea level under the United States.
IERS Reference Meridian
Satellites changed the reference from the surface of the Earth to its center of mass around which all satellites orbit regardless of surface irregularities. The first satellite navigation system, TRANSIT, selected in the 1960s as its reference meridian on an Earth-centered ellipsoid the longitude on the NAD27 ellipsoid of its development laboratory halfway between Washington, D.C. and Baltimore, Maryland. These identical numeric longitudes at a location remote from Greenwich caused 0° of longitude on an Earth-centered ellipsoid to be 5.3" east of the astronomic Greenwich prime meridian through the Airy transit circle. At the latitude of Greenwich, this amounts to 102.5 metres. This was officially accepted by the Bureau International de l'Heure (BIH) in 1984 via its BTS84 (BIH Terrestrial System) that later became WGS84 (World Geodetic System 1984) and the various ITRFs (International Terrestrial Reference Systems).
Due to the movement of Earth's tectonic plates, the line of 0° longitude along the surface of the Earth has slowly moved toward the west from this shifted position by a few centimetres, that is, towards the Airy transit circle (or the Airy transit circle has moved toward the east, depending on your point of view) since 1984 (or the 1960s). With the introduction of satellite technology, it became possible to create a more accurate and detailed global map. With these advances there also arose the necessity to define a reference meridian that, whilst being derived from the Airy transit circle, would also take into account the effects of plate movement and variations in the way that the Earth was spinning. As a result, the International Reference Meridian was established and is commonly used to denote Earth's prime meridian (0° longitude) by the International Earth Rotation and Reference Systems Service, which defines and maintains the link between longitude and time. Based on observations to satellites and celestial compact radio sources (quasars) from various coordinated stations around the globe, Airy's transit circle drifts northeast about 2.5 centimetres per year relative to this Earth-centered 0° longitude. Circa 1999 the international reference meridian (IRM) passed 5.31 arcseconds east of Airy's meridian or 102.5 metres (336.3 feet) at the latitude of the Royal Observatory, Greenwich, London. It is also the reference meridian of the Global Positioning System operated by the United States Department of Defense, and of WGS84 and its two formal versions, the ideal International Terrestrial Reference System (ITRS) and its realization, the International Terrestrial Reference Frame (ITRF). A current convention on the Earth uses the opposite of the IRM as the basis for the International Date Line.
List of places
Country, territory or sea Notes Arctic Ocean Greenland Sea Norwegian Sea North Sea United Kingdom The northernmost land on this meridian is near Tunstall in East Riding, Yorkshire.
The southernmost land in the UK is Peacehaven, East Sussex.
English Channel France The northernmost point on this meridian is in Villers-sur-Mer, Calvados.
The southernmost point is near Gavarnie.
Spain Passing just west of Monte Perdido, in the Pyrenees Mediterranean Sea Gulf of Valencia Spain Mediterranean Sea Algeria Mali Burkina Faso Togo For about 600 m Ghana For about 16 km Togo For about 39 km Ghana Passing through Lake Volta at Atlantic Ocean Passing through the Equator at Southern Ocean Antarctica Queen Maud Land, claimed by Norway
Prime meridian on other planetary bodies
As on the Earth, prime meridians must be arbitrarily defined. Often a landmark such as a crater is used, other times a prime meridian is defined by reference to another celestial object, or by magnetic fields. The prime meridians of the following planetographic systems have been defined:
- The prime meridian of the Moon lies directly in the middle of the face of the moon visible from Earth and passes near the crater Bruce.
- The prime meridian of Mars is defined by the crater Airy-0.
- The prime meridian of Venus passes through the central peak in the crater Ariadne.
- Two different heliographic coordinate systems are used on the Sun. The first is the Carrington heliographic coordinate system. In this system, the prime meridian passes through the center of the solar disk as seen from the Earth on 9 November 1853, which is when Richard Christopher Carrington started his observations of sunspots. The second is the Stonyhurst heliographic coordinates system.
- Jupiter has several coordinate systems because its cloud tops—the only part of the planet visible from space—rotate at different rates depending on latitude. It is unknown whether Jupiter has any internal solid surface that would enable a more Earth-like coordinate system. Scientific Astronomer uses System II coordinates, based on the mean atmospheric rotation of the north and south Equatorial belts. System III coordinates use Jupiter's magnetic field.
- Titan, like the Earth's moon, always has the same face towards Saturn, and so that face is 0 longitude.
Maps by prime meridian Maps in Wikimedia Commons by prime meridian
- Prime Meridian, geog.port.ac.uk
- Norgate 2006
- Hooker 2006
- e.g. Jacob Roggeveen in 1722 reported the longitude of Easter Island as 268° 45' (starting from Fuertaventura) in the Extract from the Official log of Jacob Roggeveen reproduced in Bolton Glanville Corney, ed. (1908), The voyage of Don Felipe Gonzalez to Easter Island in 1770-1, Hakluyt Society, p. 3, retrieved 13 Jan 2013
- Speech by Pierre Janssen, director of the Paris observatory, at the first session of the Meridian Conference.
- Sobel & Andrewes 1998, pp. 110–115
- Sobel & Andrewes 1998, pp. 197–199
- International Conference Held at Washington for the Purpose of Fixing a Prime Meridian and a Universal Day. October, 1884. Project Gutenberg
- Atlas do Brazil, 1909, by Barão Homem de Mello e Francisco Homem de Mello, published in Rio de Janeiro by F. Briguiet & Cia.
- Ancient, used in Ptolemy's Geographia. Later redefined 17° 39′ 46″ W of Greenwich to be exactly 20° W of Paris. French "submarin" at Washington 1884.
- The meridian of Ptolemy's Almagest.
- Wilcomb E. Washburn, "The Canary Islands and the Question of the Prime Meridian: The Search for Precision in the Measurement of the Earth"
- Maimonides, Hilchot Kiddush Hachodesh 11:17, calls this point אמצע היישוב, "the middle of the habitation", i.e. the habitable hemisphere. Evidently this was a convention accepted by Arab geographers of his day.
- Burgess c. 2013
- "International Conference Held at Washington for the Purpose of Fixing a Prime Meridian and a Universal Day. October, 1884. Protocols of the proceedings.". Project Gutenberg. 1884. Retrieved 30 November 2012.
- Greenwich Observatory ... the story of Britain's oldest scientific institution, the Royal Observatory at Greenwich and Herstmonceux, 1675-1975 p.10. Taylor & Francis, 1975
- . McCarthy, P. Kenneth; Seidelmann (2009). TIME from Earth Rotation to Atomic Physics. Weinheim: Wiley-VCH. pp. 244–5.
- ROG Learing Team (23 August 2002). "The Prime Meridian at Greenwich". Royal Museums Greenwich. Royal Museums Greenwich. Retrieved 14 June 2012.
- History of the Prime Meridian -Past and Present
- IRM on grounds of Royal Observatory from Google Earth Accessed 30 March 2012
- The astronomic latitude of the Royal Observatory is 51°28'38"N whereas its latitude on the European Terrestrial Reference Frame (1989) datum is 51°28'40.1247"N.
- Guinot, B., 2011. Solar time, legal time, time in use. Metrologica 48, S181–S185.
- "USGS Astrogeology: Rotation and pole position for the Sun and planets (IAU WGCCRE)". Retrieved 22 October 2009.
- "Carrington heliographic coordinates".
- "Planetographic Coordinates". Retrieved 2009-06-19.
- Burgess, Ebenezer (c. 2013) , "Translation of the Surya-Siddhanta", Journal of the American Oriental Society (e book) 6, Google, p. 185
- Hooker, Brian (2006), A multitude of prime meridians, retrieved 13 Jan 2013
- Norgate, Jean and Martin (2006), Prime meridian, retrieved 13 Jan 2013
- Sobel, Dava; Andrewes, William J. H. (1998), The Illustrated Longitude, Fourth Estate, London
|Wikimedia Commons has media related to: Prime meridian|
- "Where the Earth's surface begins—and ends", Popular Mechanics, December 1930
- scanned TIFFs of the conference proceedings
- Prime meridians in use in the 1880s, by country
- Canadian Prime Meridian