Glossary

WGS84World Geodetic System 1984

Short answer

The reference ellipsoid and datum used by GPS and the de-facto GNSS standard. Semi-major axis a = 6378137 m, flattening f = 1/298.257223563. Position differences from local datums (NAD83, ETRS89, GDA2020, CGCS2000) range from tens of cm to several metres depending on region.

Detailed explanation

WGS84 is the geodetic datum (reference ellipsoid + origin + orientation) used by GPS, and the de-facto GNSS standard adopted by every other constellation. It models Earth's geoid as an ellipsoid of revolution with semi-major axis a = 6,378,137 metres and flattening f = 1/298.257223563. The first eccentricity squared is e² ≈ 6.694×10⁻³.

WGS84 has been realised several times — WGS84(original) in 1984, then G730 (1994), G873 (1997), G1150 (2002), G1674 (2012), G1762 (2013), G2139 (2021). Each realisation is ~5–10 cm different from the previous; modern receivers use the latest. WGS84(G2139) is now within 1 cm of ITRF2014 at any survey point.

Local datums (NAD83 for North America, ETRS89 for Europe, GDA2020 for Australia, CGCS2000 for China, BJ54 for legacy Chinese surveying, etc.) differ from WGS84 by tens of centimetres to several metres depending on region. NAD83 vs WGS84 is ~1 m apart at the time of writing because NAD83 fixed the North American tectonic plate while WGS84 follows global motion.

GNSS receivers always compute in WGS84 and then transform to whatever datum the local survey requires using grid-shift files or 7-parameter Helmert transformations. The Coordinate Converter tool on this site does the WGS84-frame conversions (lat/lon ↔ UTM ↔ MGRS ↔ ECEF); local-datum transforms are out of scope.

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