Geoid
Builds on GeopotentialLevel setReference ellipsoid
Definition
Let be the geopotential of the Earth. The geoid is the level set where the constant is chosen so that this surface best fits mean sea level. The fit is in the least squares sense. The geoid undulation at a point of a reference ellipsoid is the height of the geoid above the ellipsoid, measured along the ellipsoid normal.
Remarks
Example: for a non-rotating Earth with spherically symmetric density, outside the Earth, so every level set there is a sphere ; the geoid would be a sphere. Non-example: the instantaneous sea surface is not the geoid, since tides, winds and currents move it away from a level surface by up to a few metres. The geoid is everywhere perpendicular to the gravity vector . The orthometric height of a point, its height above the geoid, satisfies , where is the ellipsoidal height. On the Earth, ranges roughly between m and m.
Reading path
To understand this page from the ground up, read these 7 pages in order. The foundations come first.
Show the path as a graph
- no evidence level
- Euclidean space object
- Function concept
- Geopotential concept
- Reference ellipsoid concept
- Function of several variables concept
- Level set concept
- Geoid definition
Further reading
About this page
| Tag | 2AB1XN3JQ4 |
|---|---|
| URI | m2://2AB1XN3JQ4 |
| Kind | definition |
| Writing | W0 stub |
| MSC | 86A30, 86A20 |
| Defines | Geoid |
| Uses | Geopotential, Level set, Reference ellipsoid |
| Changed | 3 November 2026 |
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