Vincenty's formulae
Builds on Geodesics on an ellipsoidFlatteningGeodetic coordinates
Definition
Let an ellipsoid have semi-major axis , flattening and semi-minor axis . Let two points have geodetic coordinates and , and set . Their reduced latitudes are . Vincenty's inverse method starts from and repeats the following steps until stops changing: With the final values, set and The output distance is . The azimuth at the first point is . Vincenty's direct method solves the direct problem with the same series and an iteration on .
Remarks
Example: for one gets , so after one step, and gives , ; then is the great-circle distance. Non-example: for some nearly antipodal pairs of points, the iteration on does not converge, so the method gives no answer. The variable is the azimuth of the geodesic where it crosses the equator, and is the arc length on the auxiliary sphere. If , both points lie on the equator and the term with is dropped.
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
- Flattening concept
- Geodesic concept
- Geodetic coordinates concept
- Great-circle distance concept
- Reference ellipsoid concept
- Geodesics on an ellipsoid problem
- Vincenty's formulae definition
Further reading
- Web https://en.wikipedia.org/wiki/Vincenty%27s_formulae, Inverse problem
About this page
| Tag | MB8EPS233V |
|---|---|
| URI | m2://MB8EPS233V |
| Kind | definition |
| Writing | W0 stub |
| MSC | 86A30, 53A05 |
| Defines | Vincenty's formulae |
| Uses | Geodesics on an ellipsoid, Flattening, Geodetic coordinates |
| Changed | 3 November 2026 |
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