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Meridian (geography)

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and Canada were also improving their railroad system and needed a standard time as well. With a standard meridian, stage coach and trains were able to be more efficient. The argument of which meridian is more scientific was set aside in order to find the most convenient for practical reasons. They were also able to agree that the universal day was going to be the mean solar day. They agreed that the days would begin at midnight and the universal day would not impact the use of local time. A report was submitted to the "Transactions of the Royal Society of Canada", dated 10 May 1894; on the "Unification of the Astronomical, Civil and Nautical Days"; which stated that:
47: 331: 144: 539:– in the late 19th century and early 20th century, most countries have adopted the standard time of one of the 24 meridians closest to their geographical position, as decided by the International Meridian Conference in 1884. Although, a few time zones are offset by an additional 30 or 45 minutes, such as in the 483:
classified this true meridian versus the magnetic meridian in order to have a more qualitative, intuitive, and abstract function. He used the true meridian since his compass varied by a few degrees. There were some variations. When he noted the sight line for the True Meridian from his family's house
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is the moment when a celestial object passes the meridian of longitude of the observer. At this point, the celestial object is at its highest point. When the Sun passes two times an altitude while rising and setting can be averaged to give the time of meridian passage. Navigators utilized the Sun's
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It was in the best interests of the nations to agree to one standard meridian to benefit their fast growing economy and production. The disorganized system they had before was not sufficient for their increasing mobility. The coach services in England had erratic timing before the GWT. United States
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The position of the prime meridian has changed a few times throughout history, mainly due to the transit observatory being built next door to the previous one (to maintain the service to shipping). Such changes had no significant practical effect. Historically, the average error in the determination
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to vote on an international prime meridian. Ultimately the outcome was as follows: there would be only one prime meridian, the prime meridian was to cross and pass at Greenwich (which was the 0°), there would be two longitude direction up to 180° (east being plus and west being minus), there will be
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in 200 BC. This prime meridian was used to provide measurement of the earth, but had many problems because of the lack of latitude measurement. Many years later around the 19th century there were still concerns of the prime meridian. Multiple locations for the geographical meridian meant that there
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Because of a growing international economy, there was a demand for a set international prime meridian to make it easier for worldwide traveling which would, in turn, enhance international trading across countries. As a result, a Conference was held in 1884, in Washington, D.C. Twenty-six countries
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Toward the ending of the 12th century there were two main locations that were acknowledged as the geographic location of the meridian, France and Britain. These two locations often conflicted and a settlement was reached only after there was an International Meridian Conference held, in which
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There were two main reasons for this. The first was that the USA had already chosen Greenwich as the basis for its own national time zone system. The second was that in the late 19th century, 72% of the world's commerce depended on sea-charts which used Greenwich as the Prime Meridian. The
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Standard meridians … They are 15° apart. The focal time on any one of them, therefore, differs exactly one hour from the local time on either of the two others between which it is situated. Each standard meridian is the middle line of a belt extending 15°
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poles and the observer. The true meridian can be found by careful astronomical observations, and the magnetic meridian is simply parallel to the compass needle. The arithmetic difference between the true and magnetic meridian is called the
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Many of these instruments rely on the ability to measure the longitude and latitude of the Earth. These instruments also were typically affected by local gravity, which paired well with existing technologies such as the magnetic meridian.
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position (measured at Greenwich). The position of the current geodetic prime meridian is not identified at all by any kind of sign or marking at Greenwich (as the older astronomic position was), but can be located using a GPS receiver.
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The declination of major stars are their angles north and south from the celestial equator. The meridian passage will not occur exactly at 12 hours because of the Earth orbit excentricity (see
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It is intended that local time at any place on the surface of the globe shall generally be regulated by the standard meridian nearest or most convenient to such place in longitude.
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Haughton, Graves Champney (1 January 1851). "On the relative dynamic value of the degrees of the compass; and on the cause of the needle resting in the magnetic meridian".
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will be parallel to the magnetic meridian. However, a compass needle will not be steady in the magnetic meridian, because of the longitude from east to west being complete
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in a circle, the meridian on the opposite side of the Earth from Greenwich, the antimeridian, forms the other half of a circle with the one through Greenwich, and is at
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is the chord that goes from one pole to the other, passing through the observer, and is contrasted with the magnetic meridian, which goes through the
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The astronomic prime meridian at Greenwich, England. The geodetic prime meridian is actually 102.478 meters east of this point since the adoption of
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Doumbia, Vafi; Boka, Kouadio; Kouassi, Nguessan; Grodji, Oswald Didier Franck; Amory-Mazaudier, Christine; Menvielle, Michel (4 January 2017).
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to the depot, he could check the declination of his compass before and after surveying throughout the day. He noted this variation down.
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recommendation was based on the argument that naming Greenwich as Longitude 0º would be of advantage to the largest number of people.
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declination and the Sun's altitude at local meridian passage, in order to calculate their latitude with the formula.
673:"So, What is Actually the Distance from the Equator to the Pole? – Overview of the Meridian Distance Approximations" 97: 351: 1105:
Principal Facts of the Earth's Magnetism and Methods of Determining the True Meridian and the Magnetic Declination
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Malys, Stephen; Seago, John H.; Pavlis, Nikolaos K.; Seidelmann, P. Kenneth; Kaplan, George H. (December 2015).
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was inconsistency, because each country had their own guidelines for where the prime meridian was located.
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First Teachings about the Earth; its lands and waters; its countries and States, etc
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a universal day, and the day begins at the mean midnight of the initial meridian.
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and the meridians from Greenwich (0°) east to the antimeridian (180°) define the
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Resources page of the U.S. Department of the Interior, Bureau of Land Management
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McLean, Albert F. (1968). "Thoreau's True Meridian: Natural Fact and Metaphor".
203:. The position of a point along the meridian is given by that longitude and its 46: 776: 2132: 2028: 1983: 875: 850: 831: 814: 758: 657: 639: 536: 524: 1371: 954: 929: 1004:
Obuchovski, Romuald; Petroškevičius, Petras; Būga, Arūnas (1 January 2008).
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Smith, Humphry M. (January 1976). "Greenwich time and the prime meridian".
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of longitude was much larger than the change in position. The adoption of
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of magnetic force lines along the surface of the Earth. Therefore, a
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Abstracts of the Papers Communicated to the Royal Society of London
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at the same time. The same Latin stem gives rise to the terms
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Withers, Charles W. J. (2017). "Ruling Space, Fixing Time".
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used to disambiguate hours of the day when utilizing the
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on Earth's surface. The length of a meridian on a modern
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is an equivalent imaginary line connecting the magnetic
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A standard meridian is a meridian used for determining
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Harper's School Geography: With Maps and Illustrations
407:- begins at midnight and ends at midnight following, 207:, measured in angular degrees north or south of the 531:. Since the adoption of time zones – as opposed to 71:. Unsourced material may be challenged and removed. 844: 842: 382:" (WGS84) as the positioning system has moved the 626:Withers, Charles W. J. (2017). "Absurd Vanity". 147:Meridians run between the North and South poles. 1303:What Shall be the Prime Meridian for the World? 500:Latitude = (90° – noon altitude + declination) 386:prime meridian 102.478 metres east of its last 318: 753:. Harvard University Press. pp. 263–274. 27:Line between the poles with the same longitude 1418: 343:Greenwich was recognized as the 0° location. 290:a.m. (ante meridiem) and p.m. (post meridiem) 8: 1261:. American Book Company. 1885. p. 129. 1425: 1411: 1403: 1360:A history of the rectangular survey system 1284:United States National Bureau of Standards 374:. Most maps show the lines of longitude. 1021: 953: 874: 830: 688: 395:Effect of Prime Meridian (Greenwich Time) 276:passes through a given meridian at solar 131:Learn how and when to remove this message 142: 1102:U.S. Coast and Geodetic Survey (1919). 615: 815:"Where exactly is the prime meridian?" 7: 69:adding citations to reliable sources 1352:The Principal Meridian Project (US) 1321:"How time zones confused the world" 1108:. U.S. Government Printing Office. 440:and can be taken as the horizontal 1279:Standard Time Throughout the World 851:"Why the Greenwich meridian moved" 30:For the astronomical concept, see 25: 348:Greenwich (inside Greenwich Park) 313:International Meridian Conference 306:International Meridian Conference 300:International Meridian Conference 1448: 1393:The New Student's Reference Work 1213:10.4159/harvard.9780674074811.c7 1180:10.4159/harvard.9780674074811.c6 1071:10.4159/harvard.9780674074811.c8 45: 1205:The Lost Art of Finding Our Way 1172:The Lost Art of Finding Our Way 1063:The Lost Art of Finding Our Way 1023:10.3846/1648-7788.2008.12.51-56 527:) is the standard meridian for 56:needs additional citations for 1242:Merriam-Webster.com Dictionary 825:(5): 5.5.2–5.5. October 2015. 1: 555:Measurement of Earth rotation 915:10.1016/0083-6656(76)90039-8 1276:Gould, Ralph Edgar (1925). 199:). In other words, it is a 167:connecting points of equal 2204: 1298:Committee on Standard Time 1207:. 2013. pp. 125–160. 1065:. 2013. pp. 161–192. 819:Astronomy & Geophysics 303: 227:. A meridian is half of a 29: 1447: 1444: 1357:White, C. Albert (1991). 1174:. 2013. pp. 99–124. 876:10.1007/s00190-015-0844-y 759:10.4159/9780674978935-011 736:"Royal Museum Greenwitch" 640:10.4159/9780674978935-004 595:Public Land Survey System 80:"Meridian" geography 1061:"The Sun and the Moon". 955:10.5194/angeo-35-39-2017 632:Harvard University Press 380:World Geodetic System 84 272:, meaning "midday"; the 1042:www.merriam-webster.com 1038:"Definition of AZIMUTH" 832:10.1093/astrogeo/atv151 671:Weintrit, Adam (2013). 364:International Date Line 197:IERS Reference Meridian 1170:"Maps and Compasses". 983:10.1098/rspl.1843.0275 690:10.12716/1001.07.02.14 350:, England, called the 339: 323: 217:Gall-Peters projection 148: 34:. For other uses, see 2188:Meridians (geography) 529:Eastern European Time 346:The meridian through 333: 268:comes from the Latin 146: 601:Dominion Land Survey 570:Meridian (astronomy) 519:. For instance, the 475:magnetic declination 454:magnetic declination 311:were present at the 65:improve this article 32:Meridian (astronomy) 1541:Tropic of Capricorn 1509:Tropic of Capricorn 1472:Tropic of Capricorn 1434:Circles of latitude 1237:"standard meridian" 946:2017AnGeo..35...39D 934:Annales Geophysicae 907:1976VA.....20..219S 895:Vistas in Astronomy 867:2015JGeod..89.1263M 225:circles of latitude 219:, each meridian is 213:Mercator projection 1245:. Merriam-Webster. 1137:American Quarterly 855:Journal of Geodesy 634:. pp. 25–72. 590:Principal meridian 521:30th meridian east 372:Eastern Hemisphere 368:Western Hemisphere 340: 286:celestial meridian 149: 2170: 2169: 1222:978-0-674-07481-1 1189:978-0-674-07481-1 1080:978-0-674-07481-1 861:(12): 1263–1272. 768:978-0-674-97893-5 720:Rosenburg, Matt. 649:978-0-674-97893-5 511:Standard meridian 430:magnetic meridian 424:Magnetic meridian 201:line of longitude 141: 140: 133: 115: 18:Standard meridian 16:(Redirected from 2195: 2161: 2154: 2147: 2140: 1551:Antarctic Circle 1536:Tropic of Cancer 1524: 1523:Antarctic Circle 1517: 1510: 1503: 1502:Tropic of Cancer 1495: 1487: 1486:Antarctic Circle 1480: 1473: 1466: 1465:Tropic of Cancer 1458: 1452: 1427: 1420: 1413: 1404: 1399: 1397: 1388: 1386:"Meridian"  1375: 1365: 1339: 1338: 1336: 1334: 1317: 1311: 1310: 1294: 1288: 1287: 1273: 1267: 1266: 1253: 1247: 1246: 1233: 1227: 1226: 1200: 1194: 1193: 1167: 1161: 1160: 1132: 1126: 1125: 1099: 1093: 1092: 1058: 1052: 1051: 1049: 1048: 1034: 1028: 1027: 1025: 1001: 995: 994: 966: 960: 959: 957: 925: 919: 918: 890: 881: 880: 878: 846: 837: 836: 834: 811: 805: 804: 802: 801: 787: 781: 780: 746: 740: 739: 732: 726: 725: 717: 711: 710: 701: 695: 694: 692: 668: 662: 661: 623: 505:Equation of time 494:meridian passage 488:Meridian passage 481:Henry D. Thoreau 411:astronomical day 195:(currently, the 136: 129: 125: 122: 116: 114: 73: 49: 41: 21: 2203: 2202: 2198: 2197: 2196: 2194: 2193: 2192: 2173: 2172: 2171: 2166: 2165: 2164: 2163: 2159: 2156: 2152: 2149: 2145: 2142: 2138: 2135: 2130: 2125: 2120: 2115: 2108: 2103: 2098: 2093: 2083: 2078: 2073: 2068: 2063: 2056: 2051: 2046: 2041: 2031: 2026: 2021: 2016: 2011: 2006: 2001: 1996: 1991: 1986: 1981: 1976: 1971: 1966: 1961: 1956: 1951: 1946: 1941: 1934: 1929: 1924: 1919: 1914: 1909: 1904: 1899: 1894: 1889: 1884: 1879: 1874: 1869: 1864: 1859: 1854: 1849: 1844: 1839: 1834: 1829: 1824: 1819: 1814: 1809: 1804: 1799: 1794: 1789: 1784: 1779: 1774: 1769: 1764: 1759: 1754: 1749: 1744: 1739: 1734: 1729: 1724: 1719: 1714: 1709: 1704: 1699: 1694: 1689: 1684: 1679: 1674: 1669: 1664: 1659: 1654: 1649: 1644: 1639: 1634: 1627: 1622: 1617: 1610: 1605: 1600: 1593: 1588: 1583: 1576: 1571: 1566: 1553: 1548: 1543: 1538: 1533: 1526: 1522: 1519: 1515: 1512: 1508: 1505: 1501: 1498: 1493: 1489: 1485: 1482: 1478: 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Index

Standard meridian
Meridian (astronomy)
Meridian

verification
improve this article
adding citations to reliable sources
"Meridian" geography
news
newspapers
books
scholar
JSTOR
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geography
geodesy
locus
longitude
angle
degrees
units
east
west
prime meridian
IERS Reference Meridian
latitude
Equator
Mercator projection
Gall-Peters projection

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