Physical geodesy
Builds on GeodesyGeopotentialPotential theory
Definition
Physical geodesy is the branch of geodesy that determines the gravity field of the Earth and its relation to the figure of the Earth. Its central unknown is the gravity potential, the geopotential , as a function on and outside the Earth's surface. Its methods are those of potential theory, applied to measurements of gravity, of the direction of the plumb line and of satellite orbits.
Remarks
Example: determining the geoid from gravity measurements by Stokes' formula is a problem of physical geodesy. Non-example: computing the distance between two points of a given ellipsoid uses no gravity data; it belongs to geometric geodesy. Physical geodesy also provides orthometric heights, which are measured from the geoid along the plumb line.
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To understand this page from the ground up, read these 4 pages in order. The foundations come first.
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- no evidence level
- Geodesy concept
- Geopotential concept
- Potential theory concept
- Physical geodesy definition
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About this page
| Tag | 5HE6079K1N |
|---|---|
| URI | m2://5HE6079K1N |
| Kind | definition |
| Writing | W0 stub |
| MSC | 86A30, 86A20 |
| Defines | Physical geodesy |
| Uses | Geodesy, Geopotential, Potential theory |
| Changed | 3 November 2026 |
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