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Geodetic Reference System 1980 information


The Geodetic Reference System 1980 (GRS80) is a geodetic reference system consisting of a global reference ellipsoid and a normal gravity model.[1][2][3]

  1. ^ Moritz, Helmut [in German] (September 1980). "Geodetic Reference System 1980" (PDF). Bulletin Géodésique. 54 (3): 395–405. Bibcode:1980BGeod..54..395M. doi:10.1007/BF02521480. S2CID 198209711.
  2. ^ Moritz, H. [in German] (1992). "Geodetic Reference System 1980". Bulletin Géodésique. 66 (2). Springer Science and Business Media LLC: 187–192. Bibcode:1992BGeod..66..187M. doi:10.1007/bf00989270. ISSN 0007-4632. S2CID 122916060.
  3. ^ Moritz, Helmut [in German] (March 2000). "Geodetic Reference System 1980" (PDF). Journal of Geodesy. 74 (1): 128–162. doi:10.1007/S001900050278. S2CID 195290884.

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Geodetic Reference System 1980

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The Geodetic Reference System 1980 (GRS80) is a geodetic reference system consisting of a global reference ellipsoid and a normal gravity model. Geodesy...

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Spatial reference system

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national grid reference system, Britain Lambert-93 (fr), the official projection in Metropolitan France Hellenic Geodetic Reference System 1987, Greece...

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The Hellenic Geodetic Reference System 1987 or HGRS87 (Greek: Ελληνικό Γεωδαιτικό Σύστημα Αναφοράς 1987 or ΕΓΣΑ'87) is a geodetic system commonly used...

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Earth ellipsoid

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Australia for the Australian Geodetic Datum and in the South American Datum 1969. The GRS-80 (Geodetic Reference System 1980) as approved and adopted by...

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Projected coordinate system

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coordinate system – also called a projected coordinate reference system, planar coordinate system, or grid reference system – is a type of spatial reference system...

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Global Area Reference System

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Geodesy

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simplest terms, the degree of central concentration of mass. The 1980 Geodetic Reference System (GRS 80), adopted at the XVII General Assembly of the International...

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Universal Transverse Mercator coordinate system

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Geographic coordinate system

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Physical geodesy

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poids; valeur conventionnelle de gn. Moritz, Helmut (2000). "Geodetic Reference System 1980". Journal of Geodesy. 74 (1): 128–133. doi:10.1007/s001900050278...

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Geoid

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position, the height of the geoid (e.g., the EGM96 geoid) over the World Geodetic System (WGS) ellipsoid. They are then able to correct the height above the...

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Equator

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radius, namely 40,075.0142 km (24,901.4594 mi). The GRS 80 (Geodetic Reference System 1980) as approved and adopted by the IUGG at its Canberra, Australia...

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Unit of length

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"Metrication in Australia" (PDF). Moritz, H. (March 2000). "Geodetic Reference System 1980". Journal of Geodesy. 74 (1): 128–133. Bibcode:2000JGeod..74...

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Gravity of Earth

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1970. If the terrain is at sea level, we can estimate, for the Geodetic Reference System 1980, g { ϕ } {\displaystyle g\{\phi \}} , the acceleration at latitude...

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Horizontal position representation

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what to consider. Rotation formalisms in three dimensions Geodetic coordinates Geodetic system Plane coordinates Gade, Kenneth (2010). "A non-singular horizontal...

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Earth radius

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Properties". arXiv:1510.07674 [astro-ph.SR]. Moritz, H. (1980). Geodetic Reference System 1980 Archived 2016-02-20 at the Wayback Machine, by resolution...

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reference ellipsoid for Earth is small, only about one part in 300. Historically, flattening was computed from grade measurements. Nowadays, geodetic...

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Geopotential

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revolution called the reference ellipsoid. The currently most widely used reference ellipsoid, that of the Geodetic Reference System 1980 (GRS80), approximates...

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