Deflection of the vertical
Builds on Reference ellipsoidGeodetic coordinatesGeopotential
Definition
Let be a point near the Earth's surface. Let and be the astronomical latitude and longitude of . They give the direction of the gravity vector of the geopotential at . Let and be the geodetic latitude and longitude of , which give the direction of the normal to the reference ellipsoid through . The deflection of the vertical at is the angle between these two directions. Its north–south component and east–west component are and for small angles .
Remarks
Example: if , and , then , , and the deflection is in the north–south direction. Non-example: the difference alone is not the east–west component; it must be multiplied by , because meridians converge towards the poles. The east–west component also links astronomical and geodetic azimuths: the Laplace equation holds to first order for a line of sight close to the horizon. It is used to control the azimuths of triangulation networks. Some authors use the opposite sign convention, with ellipsoid direction minus gravity direction.
Reading path
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
- Geodetic coordinates concept
- Geopotential concept
- Reference ellipsoid concept
- Deflection of the vertical definition
Further reading
About this page
| Tag | PPPSMTJMJP |
|---|---|
| URI | m2://PPPSMTJMJP |
| Kind | definition |
| Writing | W0 stub |
| MSC | 86A30 |
| Defines | Deflection of the vertical |
| Uses | Reference ellipsoid, Geodetic coordinates, Geopotential |
| Changed | 3 November 2026 |
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