Content deleted Content added
Rescuing 2 sources and tagging 0 as dead.) #IABot (v2.0.9.5) (AManWithNoPlan - 15934 |
|||
(11 intermediate revisions by 9 users not shown) | |||
Line 2:
{{Use British English|date=November 2019}}
{{Use dmy dates|date=November 2022}}
[[File:Kilometre definition.svg|thumb|An early definition of the [[metre]] was one ten-millionth of the [[Earth quadrant]], the distance from the [[North Pole]] to the [[Equator]], measured along a [[meridian (geography)|meridian]] through [[Paris]].]]
The '''history of the metre''' starts with the [[Scientific Revolution]] that is considered to have begun with [[Nicolaus Copernicus]]'s publication of {{lang|la|[[De revolutionibus orbium coelestium]]}} in 1543. Increasingly accurate measurements were required, and scientists looked for measures that were universal and could be based on natural phenomena rather than royal decree or physical prototypes. Rather than the various complex systems of subdivision then in use, they also preferred a decimal system to ease their calculations.
With the [[French Revolution]] (1789) came a desire to replace many features of the [[Ancien Régime]], including [[Units of measurement in France before the French Revolution|the traditional units of measure]]. As a base unit of length, many scientists had favoured the [[seconds pendulum]] (a pendulum with a half-period of one second) one century earlier, but this was rejected as it had been discovered that this length varied from place to place with local gravity. A new unit of length, the ''metre'' was introduced – defined as one ten-millionth of the shortest distance from the North Pole to the equator [[Paris meridian|passing through Paris]], assuming an Earth [[flattening]] of {{Sfrac|1
The historical French official standard of the metre was made available in the form of the {{lang|fr|[[Mètre des Archives]]}}, a platinum bar held in Paris. During the mid nineteenth century, following the [[American Revolution]] and [[Decolonization of the Americas|
The {{lang|fr|[[Mètre des Archives]]}} and its copies such as the Committee Meter were replaced from 1889 at the initiative of the [[International Association of Geodesy|International Geodetic Association]] by thirty [[platinum-iridium]] bars kept across the globe.<ref>{{Cite web|url=https://www.bipm.org/fr/measurement-units/history-si/international-metre-commission.html|title=BIPM - Commission internationale du mètre|website=www.bipm.org|access-date=13 November 2019}}</ref> A better [[standardization]] of the new prototypes of the metre and their
Progress in science finally allowed the definition of the metre to be dematerialized; thus in 1960 a new definition based on a specific number of wavelengths of light from a specific transition in [[krypton-86]] allowed the standard to be universally available by measurement. In 1983 this was updated to a length defined in terms of the [[speed of light]]; this definition was reworded in 2019:<ref name="2019metre">{{citation
Line 35 ⟶ 34:
[[Scientific revolution]] began with [[Copernicus]] work. [[Galileo]] discovered [[gravitational acceleration]] explaining the fall of bodies at the surface of the Earth. He also observed the regularity of the period of swing of the [[pendulum]] and that this period depended on the length of the pendulum. In 1645 [[Giovanni Battista Riccioli]] was the first to determine the length of a "[[seconds pendulum]]" (a [[pendulum]] with a half-period of one [[second]]).<ref name=":8">{{Cite book |last=Guedj |first=Denis |title=Le mètre du monde |date=2011 |publisher=Éd. du Seuil |isbn=9782757824900 |location=Paris |pages=38 |oclc=758713673 |author-link=Denis Guedj}}</ref>
[[Kepler's laws of planetary motion]] served both to the discovery of [[Newton's law of universal gravitation]] and to the determination of the distance from Earth to the Sun by [[Giovanni Domenico Cassini]].<ref>{{Cite book |last=Bond, Peter, (1948- ...). |title=L'exploration du système solaire |date=2014 |publisher=De Boeck |others=Dupont-Bloch, Nicolas. |isbn=9782804184964 |edition=[Édition française revue et corrigée] |location=Louvain-la-Neuve |pages=5–6 |oclc=894499177}}</ref> They both also used a determination of the size of the Earth, then considered as a sphere, by [[Jean Picard]] through [[Triangulation (surveying)|triangulation]] of [[Paris meridian]]. In 1671, Jean Picard also measured the length of a [[seconds pendulum]] at [[Paris Observatory]] and proposed this unit of measurement to be called the astronomical radius (French: ''Rayon Astronomique''). He found the value of 440.5 [[ligne]]s of the Toise of Châtelet (a {{lang|fr|[[toise]]}} [English: [[fathom]]] is defined as 6 {{lang|fr|[[Pied (unit)|pieds]]}}
[[Jean Richer]] and [[Giovanni Domenico Cassini]] measured the parallax of Mars between Paris and [[Cayenne]] in [[French Guiana]] when Mars was at its closest to Earth in 1672. They arrived at a figure for the [[solar parallax]] of 9.5 arcseconds,{{refn |group=Note |The modern value of the solar parallax is {{val|8.794143}} arcseconds.<ref name=almanac>{{citation |author=United States Naval Observatory |author-link=United States Naval Observatory |title=Selected Astronomical Constants |url=http://asa.usno.navy.mil/static/files/2018/Astronomical_Constants_2018.pdf |periodical=The Astronomical Almanac Online |year=2018 |page=K7 |access-date=20 June 2019 |archive-date=20 June 2019 |archive-url=https://web.archive.org/web/20190620170003/http://asa.usno.navy.mil/static/files/2018/Astronomical_Constants_2018.pdf |url-status=dead }}</ref>}} equivalent to an Earth–Sun distance of about 22,000 Earth radii.<ref group="Note">Since 2012 the [[astronomical unit]] has been defined as exactly {{val|149597870700}} metres or about {{convert|150|e6km|abbr=off}}.</ref> They were also the first astronomers to have access to an accurate and reliable value for the [[Earth radius|radius of Earth]], which had been measured by their colleague [[Jean Picard]] in 1669 as 3,269,000 {{lang|fr|toises}}. [[Isaac Newton]] used this measurement for establishing his [[law of universal gravitation]].<ref name="gallica">{{Cite book |last1=Biot |first1=Jean-Baptiste |url=https://gallica.bnf.fr/ark:/12148/bpt6k1510037p/f567.item |title=Recueil d'observations géodésiques, astronomiques et physiques, exécutées par ordre du Bureau des longitudes de France, en Espagne, en France, en Angleterre et en Écosse, pour déterminer la variation de la pesanteur et des degrés terrestres sur le prolongement du Méridien de Paris, faisant suite au troisième volume de la Base du Système métrique |last2=Arago |first2=François |date=1821 |pages=523, 529 |language=fr |author-link1=Jean-Baptiste Biot |author-link2=François Arago |access-date=14 September 2018 |via=[[Gallica]]}}</ref> Picard's geodetic observations had been confined to the determination of the magnitude of the earth considered as a sphere, but the discovery made by Jean Richer turned the attention of mathematicians to its deviation from a spherical form.<ref name="Bigourdan" /><ref>{{Cite book |title=L'exploration du système solaire |trans-title=The exploration of the solar system |last1=Bond |first1=Peter |last2=Dupont-Bloch |first2=Nicolas |publisher=De Boeck |year=2014 |isbn=9782804184964 |location=Louvain-la-Neuve |pages=5–6 |language=fr|oclc = 894499177}}</ref><ref>{{Cite web |url=http://350ans.obspm.fr/fr/evenement-frise/premiere-determination-distance-terre-soleil |title=Première détermination de la distance de la Terre au Soleil |trans-title=First determination of the distance from the Earth to the Sun |website=Les 350 ans de l'Observatoire de Paris |language=fr |access-date=5 September 2018}}</ref><ref>{{Cite web|url=http://adsbit.harvard.edu/full/1967LAstr..81..234G|title=1967LAstr..81..234G Page 234|website=adsbit.harvard.edu|page=237|access-date=5 September 2018}}</ref><ref>{{Cite web |url=http://clea-astro.eu/archives/web/resume.php?num_fas=100&num_art=1146 |title=INRP – CLEA – Archives : Fascicule N° 137, Printemps 2012 Les distances |trans-title=NPRI – CLEA – Archives: Issue N ° 137, Spring 2012 Distances |website=clea-astro.eu |language=fr |access-date=5 September 2018}}</ref><ref>{{Cite book|url=https://gallica.bnf.fr/ark:/12148/btv1b7300361b/f41.image|title=Mesure de la terre|last=Picard|first=Jean|author-link=Jean Picard|date=1671|via=[[Gallica]]|page=23|language=fr|access-date=5 September 2018}}</ref><ref name="Earth-figure">{{cite EB1911|wstitle=Earth, Figure of the |volume= 08 |pages= 801-813 }}</ref>
[[Christiaan Huygens]] found out the [[centrifugal force]] which explained variations of gravitational acceleration depending on latitude. He also discovered that the [[seconds pendulum]] length was a means to measure gravitational acceleration. In the 18th century, in addition
The length of the pendulum is a function of the time lapse of half a cycle <math>T_{1/2}</math>
:<math> \ell=g\left(\frac{T_{1/2}}{\pi}\right)^2. </math>
Being <math>T_{1/2}=1\ \mathrm{s}</math>, therefore <math>g={\ell\cdot \pi^2}</math>.</ref><ref group="Note">At the time the second was defined as a fraction of the Earth's rotation time and determined by clocks whose precision was checked by astronomical observations. In 1936 French and German astronomers found that Earth rotation's speed is irregular. Since 1967 atomic clocks define the second. For further information see [[atomic time]].</ref>[[File:Repsold.jpg|thumb|[[Gravimeter]] with variant of [[Repsold-Bessel pendulum]].]]According to [[Alexis Clairaut]], the study of variations in gravitational acceleration was a way to determine the [[figure of the Earth]], whose crucial parameter was the [[flattening]] of the [[Earth ellipsoid]]. In his famous work {{lang|fr|Théorie de la figure de la terre, tirée des principes de l'hydrostatique}} ('Theory of the Figure of the Earth, drawn from the Principles of Hydrostatics') published in 1743, [[Alexis Clairaut|Alexis Claude Clairaut]] synthesized the relationships existing between gravity and the shape of the Earth. Clairaut exposed there his [[Clairaut's theorem|theorem]] which established a relationship between [[gravity]] measured at different latitudes and the flattening of the Earth considered as a [[spheroid]] composed of concentric layers of variable densities. Towards the end of the 18th century, the geodesists sought to reconcile the values of flattening drawn from the measurements of meridian arcs with that given by Clairaut's spheroid drawn from the measurement of gravity. In 1789, [[Pierre-Simon de Laplace]] obtained by a calculation taking into account the measures of meridian arcs known at the time a flattening of {{Sfrac|1
Significant improvements in gravity measuring instruments must also be attributed to Bessel. He devised a gravimeter constructed by [[Adolf Repsold]] which was first used in [[Switzerland]] by [[Emile Plantamour]], [[Charles Sanders Peirce]] and Isaac-Charles Élisée Cellérier (8.01.1818 – 2.10.1889), a [[Geneva]]n mathematician soon independently discovered a mathematical formula to correct [[Observational error|systematic errors]] of this device which had been noticed by Plantamour and [[Adolphe Hirsch]].<ref>{{citation-attribution|{{Cite book|url=http://www.rac.es/ficheros/Discursos/DR_20080825_173.pdf|title=Discursos leidos ante la Real Academia de Ciencias Exactas Fisicas y Naturales en la recepcion pública de Don Joaquin Barraquer y Rovira|last=Ibáñez e Ibáñez de Ibero|first=Carlos|publisher=Imprenta de la Viuda e Hijo de D.E. Aguado|year=1881|location=Madrid|pages=70–78}}}}</ref><ref>{{Cite journal |date=1880 |title=Rapport de M. Faye sur un Mémoire de M. Peirce concernant la constance de la pesanteur à Paris et les corrections exigées par les anciennes déterminations de Borda et de Biot |url=https://gallica.bnf.fr/ark:/12148/bpt6k3047v/f1457.image.r=1880%201880 |journal=[[Comptes rendus hebdomadaires des séances de l'Académie des sciences]] |volume=90 |pages=1463–1466 |access-date=2018-10-10 |via=[[Gallica]]}}</ref> This would allow [[Friedrich Robert Helmert]] to determine a remarkably accurate value of {{Sfrac|1
[[File:Anglo-French survey of 1784-1790.jpg|thumb|upright=1.5|Triangulation of the [[Anglo-French Survey (1784–1790)]]|left]]In the 18th century, geodetic surveys found practical applications in [[French cartography]] and in the [[Anglo-French Survey (1784–1790)|Anglo-French Survey]], which aimed to connect [[Paris Observatory|Paris]] and [[Royal Observatory, Greenwich|Greenwich]] Observatories and led to the [[Principal Triangulation of Great Britain]].<ref name="Murdin">{{Cite book|url=http://public.eblib.com/choice/publicfullrecord.aspx?p=418081|title=Full meridian of glory: perilous adventures in the competition to measure the Earth|last=Murdin|first=Paul|date=2009|publisher=Copernicus Books/Springer|isbn=9780387755342|location=New York; London|language=en}}</ref><ref>{{Cite journal|last1=Martin|first1=Jean-Pierre|last2=McConnell|first2=Anita|date=20 December 2008|title=Joining the observatories of Paris and Greenwich|journal=Notes and Records of the Royal Society|language=en|volume=62|issue=4|pages=355–372|doi=10.1098/rsnr.2008.0029|issn=0035-9149|doi-access=free}}</ref> The unit of length used by the French was the {{lang|fr|Toise de Paris}}, while the English one was the [[yard]], which became the geodetic unit used in the [[British Empire]].<ref>{{Cite journal |last=Portet |first=Pierre |publisher=Laboratoire de Médiévistique Occidentale de Paris |date=2011 |title=La mesure de Paris |trans-title=The measure of Paris |url=https://halshs.archives-ouvertes.fr/halshs-01672844 |language=fr |via=Sciences de l'Homme et de la Société}}</ref><ref name="clarke">{{Cite journal |last1=Clarke |first1=Alexander Ross |last2=James |first2=Henry |date=1 January 1873 |title=XIII. Results of the comparisons of the standards of length of England, Austria, Spain, United States, Cape of Good Hope, and of a second Russian standard, made at the Ordnance Survey Office, Southampton. With a preface and notes on the Greek and Egyptian measures of length by Sir Henry James |journal=Philosophical Transactions of the Royal Society of London |language=en |volume=163 |pages=445–469 |doi=10.1098/rstl.1873.0014 |issn=0261-0523 |doi-access=free}}</ref><ref name="Ross-1867-01-01">{{Cite journal |last=Clarke |first=Alexander Ross |date=1 January 1867 |title=X. Abstract of the results of the comparisons of the standards of length of England, France, Belgium, Prussia, Russia, India, Australia, made at the ordnance Survey Office, Southampton |journal=Philosophical Transactions of the Royal Society of London |language=en |volume=157 |pages=161–180 |doi=10.1098/rstl.1867.0010 |issn=0261-0523 |s2cid=109333769}}</ref>
Line 56 ⟶ 55:
[[File:Dunkerque Belfort.JPG|thumb|upright=1.2|The [[Bell tower|belfry]] of the [[Church of Saint-Éloi, Dunkirk]] – the northern end of the [[meridian arc]] running south to [[Barcelona]]]][[File:Castell de Montjuic - Fossat entrada - Barcelona (Catalonia).jpg|thumb|upright=1.2|[[Montjuïc Castle]] in [[Barcelona]], Spain – the southern end of the meridian arc|left]]
The question of measurement reform was placed in the hands of the [[Academy of Sciences (France)|Academy of Sciences]], who appointed a commission chaired by [[Jean-Charles de Borda]]. Instead of the seconds pendulum method, the commission of the French Academy of Sciences – whose members included [[Jean-Charles de Borda|Borda]], [[Joseph-Louis Lagrange|Lagrange]], [[Pierre-Simon Laplace|Laplace]], [[Gaspard Monge|Monge]] and [[Marquis de Condorcet|Condorcet]] – decided that the new measure should be equal to one ten-millionth of the distance from the North Pole to the Equator (the quadrant of the Earth's circumference), measured along the meridian passing through Paris. Apart from the obvious consideration of safe access for French surveyors, the Paris meridian was also a sound choice for scientific reasons: a portion of the quadrant from Dunkirk to Barcelona (about 1000 km, or one-tenth of the total) could be surveyed with start- and end-points at sea level, and that portion was roughly in the middle of the quadrant, where the effects of the Earth's oblateness were expected not to have to be accounted for. The expedition would take place after the [[Anglo-French Survey (1784–1790)|Anglo-French Survey]], thus the French meridian arc, which would extend northwards across the United Kingdom, would also extend southwards to Barcelona, later to [[Balearic Islands]]. [[Jean-Baptiste Biot]] and [[François Arago]] would publish in 1821 their observations completing those of Delambre and Mechain. It was an account of the length's variation of the degrees of latitude along the Paris meridian as well as the account of the variation of the seconds pendulum's length along the same meridian between [[Shetland]] and the Baleares.<ref name="gallica" /> Improvements in the measuring devices designed by Borda and used for this survey also raised hopes for a more accurate determination of the length of this meridian arc.<ref name="RNMF">{{Cite web |title=L'histoire des unités {{!}} Réseau National de la Métrologie Française |url=https://metrologie-francaise.lne.fr/fr/metrologie/histoire-des-unites |access-date=2023-10-06 |website=metrologie-francaise.lne.fr}}</ref><ref>{{Cite book |last1=Biot |first1=Jean-Baptiste (1774-1862) Auteur du texte |url=https://gallica.bnf.fr/ark:/12148/bpt6k1510037p |title=Recueil d'observations géodésiques, astronomiques et physiques, exécutées par ordre du Bureau des longitudes de France en Espagne, en France, en Angleterre et en Écosse, pour déterminer la variation de la pesanteur et des degrés terrestres sur le prolongement du méridien de Paris... rédigé par MM. Biot et Arago,... |last2=Arago |first2=François (1786-1853) Auteur du texte |date=1821 |pages=viii-ix |language=EN}}</ref><ref name="Débarbat-1799">{{Cite web |last=Suzanne |first=Débarbat |title=Fixation de la longueur définitive du mètre |url=https://francearchives.gouv.fr/fr/pages_histoire/39436 |access-date=2023-10-06 |website=FranceArchives |language=fr}}</ref><ref name="Levallois2">{{Cite web |last=Levallois |first=Jean-Jacques |date=1986 |title=La Vie des sciences |url=https://gallica.bnf.fr/ark:/12148/bpt6k5470853s |access-date=2019-05-13 |website=Gallica |pages=288–290, 269, 276–277, 283 |language=FR}}</ref><ref>{{Cite book |last=Capderou |first=Michel |url=https://books.google.com/books?id=jRQXQhRSrz4C |title=Satellites : de Kepler au GPS |date=2011-10-31 |publisher=Springer Science & Business Media |isbn=978-2-287-99049-6 |pages=46 |language=fr}}</ref><ref>{{Cite web |last=Ramani |first=Madhvi |title=How France created the metric system |url=http://www.bbc.com/travel/story/20180923-how-france-created-the-metric-system |access-date=2019-05-21 |website=www.bbc.com |language=en}}</ref><ref>Jean-Jacques Levallois, La méridienne de Dunkerque à Barcelone et la détermination du mètre (1792 – 1799), Vermessung, Photogrammetrie, Kulturtechnik, 89 (1991), 375-380.</ref><ref name="Levallois-19912">{{Cite journal |last=Zuerich |first=ETH-Bibliothek |year=1991 |title=La méridienne de Dunkerque à Barcelone et la déterminiation du mètre (1972-1799) |url=https://dx.doi.org/10.5169/seals-234595 |language=FR |pages=377–378 |doi=10.5169/seals-234595 |access-date=2021-10-12 |website=E-Periodica}}</ref><ref name="Martin-20082">{{Cite journal |last1=Martin |first1=Jean-Pierre |last2=McConnell |first2=Anita |date=2008-12-20 |title=Joining the observatories of Paris and Greenwich |url=https://royalsocietypublishing.org/doi/10.1098/rsnr.2008.0029 |journal=Notes and Records of the Royal Society |language=en |volume=62 |issue=4 |pages=355–372 |doi=10.1098/rsnr.2008.0029 |s2cid=143514819 |issn=0035-9149}}</ref>[[File:Reflecting circle-CnAM 1842-IMG 4998-gradient.jpg|left|thumb|[[Repeating circle]] devised by [[Jean-Charles de Borda]] and constructed by [[Étienne Lenoir (instrument maker)|Étienne Lenoir]]]]
Borda was an avid supporter of [[decimalisation]]: he had invented the "[[repeating circle]]", a surveying instrument which allowed a much-improved precision in the measurement of angles between landmarks, but insisted that two different version of the device be calibrated one in [[degree (angle)|degree]]s and another in "''[[grad (angle)|grade]]s''" ({{frac|100}} of a quarter-circle), with 100 minutes to a ''grade'' and 100 seconds to a minute.<ref>{{cite web | title = Jean Charles de Borda | url = http://www-history.mcs.st-andrews.ac.uk/Biographies/Borda.html | first1=J. J. | last1=O'Connor| first2=E. F. | last2=Robertson | date = April 2003 | publisher=School of Mathematics and Statistics, University of St. Andrews, Scotland | access-date = 13 October 2015}}</ref>
Line 87 ⟶ 86:
==International prototype metre==
<!-- Various redirects link here -->
After the [[French Revolution]], [[Napoleonic Wars]] led to the adoption of the metre in [[Latin America]] following [[Decolonization|independence]] of [[Empire of Brazil|Brazil]] and [[Hispanic America]], while the [[American Revolution]] prompted the foundation of the [[United States Coast and Geodetic Survey|Survey of the Coast]] in 1807 and the creation of the [[National Institute of Standards and Technology|Office of Standard Weights and Measures]] in 1830. During the mid nineteenth century, following the defeat and expulsion of [[Napoleon|Napoleon Bonaparte]]'s forces which brought an end to the short-lived [[French campaign in Egypt and Syria|French occupation of Lower Egypt]], the metre was adopted in [[Khedivate of Egypt]] an
The intimate relationships that necessarily existed between [[metrology]] and [[geodesy]] explain that the [[International Association of Geodesy]], founded to combine the geodetic operations of different countries, in order to reach a new and more exact determination of the shape and dimensions of the Globe, prompted the project of reforming the foundations of the [[metric system]], while expanding it and making it international. Not, as it was mistakenly assumed for a certain time, that the Association had the unscientific thought of modifying the length of the metre, in order to conform exactly to its historical definition according to the new values that would be found for the terrestrial meridian. But, busy combining the arcs measured in the different countries and connecting the neighbouring triangulations, geodesists encountered, as one of the main difficulties, the unfortunate uncertainty which reigned over the equations of the units of length used. [[Adolphe Hirsch]], General [[Johann Jacob Baeyer|Baeyer]] and Colonel [[Carlos Ibáñez e Ibáñez de Ibero|Ibáñez]] decided, in order to make all the standards comparable, to propose to the Association to choose the metre for geodetic unit, and to create an international prototype metre differing as little as possible from the {{lang|fr|mètre des Archives.}}<ref>{{Cite book |last=commission |first=Internationale Erdmessung Permanente |url=https://play.google.com/store/books/details?id=M1PnAAAAMAAJ |title=Comptes-rendus des séances de la Commission permanente de l'Association géodésique internationale réunie à Florence du 8 au 17 octobre 1891 |date=1892 |publisher=De Gruyter, Incorporated |isbn=978-3-11-128691-4 |pages=99–107 |language=fr}}</ref> In 1867, the General Conference of the European Arc Measurement (German: {{lang|de|[[International Association of Geodesy|Europäische Gradmessung]]}}) called for the creation of a new, ''international prototype metre'' (IPM) and the arrangement of a system where national standards could be compared with it. The French government gave practical support to the creation of an International Metre Commission, which met in Paris in 1870 and again in 1872 with the participation of about thirty countries.<ref name="MComm">{{cite book |url=http://www.bipm.org/en/si/history-si/commission.html |title=The International Metre Commission (1870–1872) |publisher=International Bureau of Weights and Measures |access-date=15 August 2010}}</ref>{{Excerpt|Metre|International prototype metre bar|paragraphs=2-8}}
The [[Metre Convention]] was signed on 20 May 1875 in Paris and the [[International Bureau of Weights and Measures]] was created under the supervision of the [[International Committee for Weights and Measures]]. At the session on 12 October 1872 of the Permanent Committee of the International Metre Commission, which was to become the [[General Conference on Weights and Measures|International Committee for Weights and Measures]], Carlos Ibáñez e Ibáñez de Ibero had been elected president.<ref name="MComm" /><ref name="BIPMhist">{{citation |title=The BIPM and the evolution of the definition of the metre |url=http://www.bipm.org/en/measurement-units/history-si/evolution-metre.html |access-date=30 August 2016 |publisher=[[International Bureau of Weights and Measures]]}}</ref><ref name="IAG-history">{{Cite web |title=A Note on the History of the IAG |url=http://www.iag-aig.org/index.php?tpl=text&id_c=80&id_t=143 |access-date=19 September 2018 |website=IAG Homepage}}</ref><ref>{{Cite journal |last=Torge |first=W. |date=1 April 2005 |title=The International Association of Geodesy 1862 to 1922: from a regional project to an international organization |journal=Journal of Geodesy |language=en |volume=78 |issue=9 |pages=558–568 |bibcode=2005JGeod..78..558T |doi=10.1007/s00190-004-0423-0 |issn=1432-1394 |s2cid=120943411}}</ref><ref>{{Cite book |url=https://play.google.com/books/reader?id=XktTAAAAcAAJ&hl=fr&pg=GBS.PA153 |title=Procès-verbaux: Commission Internationale du Mètre. Réunions générales de 1872 |date=1872 |publisher=Imprim. Nation |pages=153–155 |language=fr}}</ref> His presidency was confirmed at the first meeting of the International Committee for Weights and Measures, on 19 April 1875. Three other members of the committee, the German astronomer, [[Wilhelm Julius Foerster]], director of the [[Berlin Observatory]] and director of the German Weights and Measures Service, the Swiss [[meteorologist]] and [[physicist]], [[Heinrich von Wild]] representing Russia, and the Swiss geodesist of German origin, Adolphe Hirsch were also among the main architects of the Metre Convention.<ref name=":3">{{Cite journal |last1=Débarbat |first1=Suzanne |last2=Quinn |first2=Terry |date=1 January 2019 |title=Les origines du système métrique en France et la Convention du mètre de 1875, qui a ouvert la voie au Système international d'unités et à sa révision de 2018 |journal=Comptes Rendus Physique |series=The new International System of Units / Le nouveau Système international d’unités |language=fr |volume=20 |issue=1 |pages=6–21 |bibcode=2019CRPhy..20....6D |doi=10.1016/j.crhy.2018.12.002 |issn=1631-0705 |doi-access=free}}</ref><ref>{{Cite book |last=COMITÉ INTERNATIONAL DES POIDS ET MESURES. |url=https://play.google.com/store/books/details?id=QgkAAAAAMAAJ |title=PROCÈS-VERBAUX DES SÉANCES DE 1875-1876. |publisher=Gauthier-Villars |year=1876 |location=Paris |pages=3}}</ref><ref name=":0">{{Cite book |last=COMlTÉ INTERNATIONAL DES POIDS ET MESURES. |title=PROCÈS-VERBAUX DES SÉANCES. DEUXIÈME SÉRIE. TOME II. SESSION DE 1903. |publisher=GAUTHIER-VILLARS |year=1903 |location=Paris |pages=5–7}}</ref> In the 1870s, [[German Empire]] played a pivotal role in the unification of the metric system through the [[International Association of Geodesy|European Arc Measurement]] but its overwhelming influence was mitigated by that of neutral states. While the German astronomer [[Wilhelm Julius Foerster]]
In recognition of France's role in designing the metric system, the BIPM is based in [[Sèvres]], just outside Paris. However, as an international organisation, the BIPM is under the ultimate control of a diplomatic conference, the ''{{lang|fr|[[Conférence générale des poids et mesures]]}}'' (CGPM) rather than the French government.<ref name="Nelson" /><ref>Article 3, [[Metre Convention]].</ref>
|