GRS80

E859784

GRS80 is a geodetic reference ellipsoid defined in 1980 that serves as a standard mathematical model of the Earth's shape for modern mapping and surveying systems.

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Statements (48)

Predicate Object
instanceOf Earth ellipsoid model
geodetic reference ellipsoid
abbreviation GRS 80 NERFINISHED
angularVelocity 7.292115e-5 rad/s
basisFor ETRS89
NAD83
many modern national datums
category geodesy
reference systems
coordinateSystem geocentric Cartesian
geodetic latitude-longitude-height
datumRole ellipsoid for global reference systems
definedInYear 1980
definingOrganization IAG NERFINISHED
International Association of Geodesy NERFINISHED
dynamicalFormFactorJ2 0.00108263
epoch 1980.0
equatorialRadius 6378137.0 m
flattening 0.00335281068118
flatteningDefinition (a−b)/a
fullName Geodetic Reference System 1980 NERFINISHED
geocentricGravitationalConstant 3.986005e14 m^3/s^2
hasParameter angular velocity
geocentric gravitational constant
inverse flattening
normal gravity formula
semi-major axis
inverseFlattening 298.257222101
normalGravityAtEquator 9.7803267715 m/s^2
normalGravityAtPole 9.8321863685 m/s^2
polarRadius 6356752.314140356 m
referenceFrameUsage global geodesy
region Earth NERFINISHED
relatedStandard IAG Geodetic Reference System 1980 resolution NERFINISHED
replaced GRS67
scope global
semiMajorAxis 6378137.0 m
semiMajorAxisUnit metre
semiMinorAxis 6356752.314140356 m
semiMinorAxisUnit metre
similarTo WGS84 ellipsoid NERFINISHED
status current
symmetry axisymmetric
type oblate spheroid
usedFor coordinate reference systems
geodetic computations
mapping
surveying

Referenced by (1)

Full triples — surface form annotated when it differs from this entity's canonical label.