In mathematics—specifically, in differential geometry—a geodesic map (or geodesic mapping or geodesic diffeomorphism) is a function that "preserves geodesics". More precisely, given two (pseudo-)Riemannian manifolds (M, g) and (N, h), a function à: M â N is said to be a geodesic map if
- ÃÂ is a diffeomorphism of M onto N; and
- the image under ÃÂ of any geodesic arc in M is a geodesic arc in N; and
- the image under the inverse function ÃÂ<sup>−1</sup> of any geodesic arc in N is a geodesic arc in M.
Examples
- If (M, g) and (N, h) are both the n-dimensional Euclidean space E<sup>n</sup> with its usual flat metric, then any Euclidean isometry is a geodesic map of E<sup>n</sup> onto itself.
- Similarly, if (M, g) and (N, h) are both the n-dimensional unit sphere S<sup>n</sup> with its usual round metric, then any isometry of the sphere is a geodesic map of S<sup>n</sup> onto itself.
- If (M, g) is the unit sphere S<sup>n</sup> with its usual round metric and (N, h) is the sphere of radius 2 with its usual round metric, both thought of as subsets of the ambient coordinate space R<sup>n+1</sup>, then the "expansion" map à: R<sup>n+1</sup> â R<sup>n+1</sup> given by ÃÂ(x) = 2x induces a geodesic map of M onto N.
- There is no geodesic map from the Euclidean space E<sup>n</sup> onto the unit sphere S<sup>n</sup>, since they are not homeomorphic, let alone diffeomorphic.
- The gnomonic projection of the hemisphere to the plane is a geodesic map as it takes great circles to lines and its inverse takes lines to great circles.
- Let (D, g) be the unit disc D â R<sup>2</sup> equipped with the Euclidean metric, and let (D, h) be the same disc equipped with a hyperbolic metric as in the Poincaré disc model of hyperbolic geometry. Then, although the two structures are diffeomorphic via the identity map i : D â D, i is not a geodesic map, since g-geodesics are always straight lines in R<sup>2</sup>, whereas h-geodesics can be curved.
- On the other hand, when the hyperbolic metric on D is given by the Klein model, the identity i : D â D is a geodesic map, because hyperbolic geodesics in the Klein model are (Euclidean) straight line segments.
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