geoid96
Well-Known Member
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..... The geoid WGS-84 was agreed in 1984, it was and still is the reference Geoid for GPS.......
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Being pedantic, WGS84 is not a geoid it is a geodetic datum. Its origin is the best estimate of the centre of the earths mass and its axes are defined by definitions of the zero meridian and polar axes. Associated with this is the WGS84 ellipsoid. This has semi-major and minors axes aimed at providing the best global estimate of mean sea level. In practice, and due to variations in density and topography, MSL can vary more than 80m above or below this ellipsoid.
The geoid is a model of the deviations of MSL from the reference ellipsoid. Most GPS receivers will output WGS84 latitude and longitude plus MSL height and the geoid separation as part of the NMEA GGA message.
Until very recently the global geoid model associated with WGS84 was EGM96. Last month this was updated by a refined model known as EGM2008.
..... The geoid WGS-84 was agreed in 1984, it was and still is the reference Geoid for GPS.......
[/ QUOTE ]
Being pedantic, WGS84 is not a geoid it is a geodetic datum. Its origin is the best estimate of the centre of the earths mass and its axes are defined by definitions of the zero meridian and polar axes. Associated with this is the WGS84 ellipsoid. This has semi-major and minors axes aimed at providing the best global estimate of mean sea level. In practice, and due to variations in density and topography, MSL can vary more than 80m above or below this ellipsoid.
The geoid is a model of the deviations of MSL from the reference ellipsoid. Most GPS receivers will output WGS84 latitude and longitude plus MSL height and the geoid separation as part of the NMEA GGA message.
Until very recently the global geoid model associated with WGS84 was EGM96. Last month this was updated by a refined model known as EGM2008.