Geodesic
In differential geometry, a geodesic (/ˌdʒiːəˈdɛsɪk,
The term "geodesic" comes from geodesy, the science of measuring the size and shape of Earth. In the original sense, a geodesic was the shortest route between two points on the Earth's surface. For a spherical Earth, it is a segment of a great circle. The term has been generalized to include measurements in much more general mathematical spaces; for example, in graph theory, one might consider a geodesic between two vertices/nodes of a graph.
In a Riemannian manifold or submanifold geodesics are characterised by the property of having vanishing geodesic curvature. More generally, in the presence of an affine connection, a geodesic is defined to be a curve whose tangent vectors remain parallel if they are transported along it. Applying this to the LeviCivita connection of a Riemannian metric recovers the previous notion.
Geodesics are of particular importance in general relativity. Timelike geodesics in general relativity describe the motion of free falling test particles.
Contents
IntroductionEdit
The shortest path between two given points in a curved space, assumed to be a differential manifold, can be defined by using the equation for the length of a curve (a function f from an open interval of R to the space), and then minimizing this length between the points using the calculus of variations. This has some minor technical problems, because there is an infinite dimensional space of different ways to parameterize the shortest path. It is simpler to restrict the set of curves to those that are parameterized "with constant speed" 1, meaning that the distance from f(s) to f(t) along the curve equals s−t. Equivalently, a different quantity may be used, termed the energy of the curve; minimizing the energy leads to the same equations for a geodesic (here "constant velocity" is a consequence of minimization).^{[citation needed]} Intuitively, one can understand this second formulation by noting that an elastic band stretched between two points will contract its length, and in so doing will minimize its energy. The resulting shape of the band is a geodesic.
It is possible that several different curves between two points minimize the distance, as is the case for two diametrically opposite points on a sphere. In such a case, any of these curves is a geodesic.
A contiguous segment of a geodesic is again a geodesic.
In general, geodesics are not the same as "shortest curves" between two points, though the two concepts are closely related. The difference is that geodesics are only locally the shortest distance between points, and are parameterized with "constant speed". Going the "long way round" on a great circle between two points on a sphere is a geodesic but not the shortest path between the points. The map t → t^{2} from the unit interval on the real number line to itself gives the shortest path between 0 and 1, but is not a geodesic because the velocity of the corresponding motion of a point is not constant.
Geodesics are commonly seen in the study of Riemannian geometry and more generally metric geometry. In general relativity, geodesics in spacetime describe the motion of point particles under the influence of gravity alone. In particular, the path taken by a falling rock, an orbiting satellite, or the shape of a planetary orbit are all geodesics in curved spacetime. More generally, the topic of subRiemannian geometry deals with the paths that objects may take when they are not free, and their movement is constrained in various ways.
This article presents the mathematical formalism involved in defining, finding, and proving the existence of geodesics, in the case of Riemannian and pseudoRiemannian manifolds. The article geodesic (general relativity) discusses the special case of general relativity in greater detail.
ExamplesEdit
The most familiar examples are the straight lines in Euclidean geometry. On a sphere, the images of geodesics are the great circles. The shortest path from point A to point B on a sphere is given by the shorter arc of the great circle passing through A and B. If A and B are antipodal points, then there are infinitely many shortest paths between them. Geodesics on an ellipsoid behave in a more complicated way than on a sphere; in particular, they are not closed in general (see figure).
Metric geometryEdit
In metric geometry, a geodesic is a curve which is everywhere locally a distance minimizer. More precisely, a curve γ : I → M from an interval I of the reals to the metric space M is a geodesic if there is a constant v ≥ 0 such that for any t ∈ I there is a neighborhood J of t in I such that for any t_{1}, t_{2} ∈ J we have
This generalizes the notion of geodesic for Riemannian manifolds. However, in metric geometry the geodesic considered is often equipped with natural parameterization, i.e. in the above identity v = 1 and
If the last equality is satisfied for all t_{1}, t_{2} ∈ I, the geodesic is called a minimizing geodesic or shortest path.
In general, a metric space may have no geodesics, except constant curves. At the other extreme, any two points in a length metric space are joined by a minimizing sequence of rectifiable paths, although this minimizing sequence need not converge to a geodesic.
Riemannian geometryEdit
In a Riemannian manifold M with metric tensor g, the length of a continuously differentiable curve γ : [a,b] → M is defined by
The distance d(p, q) between two points p and q of M is defined as the infimum of the length taken over all continuous, piecewise continuously differentiable curves γ : [a,b] → M such that γ(a) = p and γ(b) = q. In Riemannian geometry, all geodesics are locally distanceminimizing paths, but the converse is not true. In fact, only paths that are both locally distance minimizing and parameterized proportionately to arclength are geodesics. Another equivalent way of defining geodesics on a Riemannian manifold, is to define them as the minima of the following action or energy functional
Note that all minima of E are also minima of L, but L is a bigger set since paths that are minima of L can be arbitrarily reparameterized, while minima of E cannot. For a piecewise curve (more generally, a curve), the Cauchy–Schwarz inequality gives
with equality if and only if is equal to a constant a.e. It happens that minimizers of also minimize , because they turn out to be affinely parameterized, and the inequality is an equality. The usefulness of this approach is that the problem of seeking minimizers of E is a more robust variational problem. Indeed, E is a "convex function" of , so that within each isotopy class of "reasonable functions", one ought to expect existence, uniqueness, and regularity of minimizers. In contrast, "minimizers" of the functional are generally not very regular, because arbitrary reparameterizations are allowed.
The Euler–Lagrange equations of motion for the functional E are then given in local coordinates by
where are the Christoffel symbols of the metric. This is the geodesic equation, discussed below.
Calculus of variationsEdit
Techniques of the classical calculus of variations can be applied to examine the energy functional E. The first variation of energy is defined in local coordinates by
The critical points of the first variation are precisely the geodesics. The second variation is defined by
In an appropriate sense, zeros of the second variation along a geodesic γ arise along Jacobi fields. Jacobi fields are thus regarded as variations through geodesics.
By applying variational techniques from classical mechanics, one can also regard geodesics as Hamiltonian flows. They are solutions of the associated Hamilton equations, with (pseudo)Riemannian metric taken as Hamiltonian.
Affine geodesicsEdit
A geodesic on a smooth manifold M with an affine connection ∇ is defined as a curve γ(t) such that parallel transport along the curve preserves the tangent vector to the curve, so

(1)
at each point along the curve, where is the derivative with respect to . More precisely, in order to define the covariant derivative of it is necessary first to extend to a continuously differentiable vector field in an open set. However, the resulting value of (1) is independent of the choice of extension.
Using local coordinates on M, we can write the geodesic equation (using the summation convention) as
where are the coordinates of the curve γ(t) and are the Christoffel symbols of the connection ∇. This is an ordinary differential equation for the coordinates. It has a unique solution, given an initial position and an initial velocity. Therefore, from the point of view of classical mechanics, geodesics can be thought of as trajectories of free particles in a manifold. Indeed, the equation means that the acceleration vector of the curve has no components in the direction of the surface (and therefore it is perpendicular to the tangent plane of the surface at each point of the curve). So, the motion is completely determined by the bending of the surface. This is also the idea of general relativity where particles move on geodesics and the bending is caused by the gravity.
Existence and uniquenessEdit
The local existence and uniqueness theorem for geodesics states that geodesics on a smooth manifold with an affine connection exist, and are unique. More precisely:
 For any point p in M and for any vector V in T_{p}M (the tangent space to M at p) there exists a unique geodesic : I → M such that
 and
 where I is a maximal open interval in R containing 0.
In general, I may not be all of R as for example for an open disc in R^{2}. The proof of this theorem follows from the theory of ordinary differential equations, by noticing that the geodesic equation is a secondorder ODE. Existence and uniqueness then follow from the Picard–Lindelöf theorem for the solutions of ODEs with prescribed initial conditions. γ depends smoothly on both p and V.
Geodesic flowEdit
Geodesic flow is a local Raction on the tangent bundle TM of a manifold M defined in the following way
where t ∈ R, V ∈ TM and denotes the geodesic with initial data . Thus, (V) = exp(tV) is the exponential map of the vector tV. A closed orbit of the geodesic flow corresponds to a closed geodesic on M.
On a (pseudo)Riemannian manifold, the geodesic flow is identified with a Hamiltonian flow on the cotangent bundle. The Hamiltonian is then given by the inverse of the (pseudo)Riemannian metric, evaluated against the canonical oneform. In particular the flow preserves the (pseudo)Riemannian metric , i.e.
In particular, when V is a unit vector, remains unit speed throughout, so the geodesic flow is tangent to the unit tangent bundle. Liouville's theorem implies invariance of a kinematic measure on the unit tangent bundle.
Geodesic sprayEdit
The geodesic flow defines a family of curves in the tangent bundle. The derivatives of these curves define a vector field on the total space of the tangent bundle, known as the geodesic spray.
More precisely, an affine connection gives rise to a splitting of the double tangent bundle TTM into horizontal and vertical bundles:
The geodesic spray is the unique horizontal vector field W satisfying
at each point v ∈ TM; here π_{∗} : TTM → TM denotes the pushforward (differential) along the projection π : TM → M associated to the tangent bundle.
More generally, the same construction allows one to construct a vector field for any Ehresmann connection on the tangent bundle. For the resulting vector field to be a spray (on the deleted tangent bundle TM \ {0}) it is enough that the connection be equivariant under positive rescalings: it need not be linear. That is, (cf. Ehresmann connection#Vector bundles and covariant derivatives) it is enough that the horizontal distribution satisfy
for every X ∈ TM \ {0} and λ > 0. Here d(S_{λ}) is the pushforward along the scalar homothety A particular case of a nonlinear connection arising in this manner is that associated to a Finsler manifold.
Affine and projective geodesicsEdit
Equation (1) is invariant under affine reparameterizations; that is, parameterizations of the form
where a and b are constant real numbers. Thus apart from specifying a certain class of embedded curves, the geodesic equation also determines a preferred class of parameterizations on each of the curves. Accordingly, solutions of (1) are called geodesics with affine parameter.
An affine connection is determined by its family of affinely parameterized geodesics, up to torsion (Spivak 1999, Chapter 6, Addendum I). The torsion itself does not, in fact, affect the family of geodesics, since the geodesic equation depends only on the symmetric part of the connection. More precisely, if are two connections such that the difference tensor
is skewsymmetric, then and have the same geodesics, with the same affine parameterizations. Furthermore, there is a unique connection having the same geodesics as , but with vanishing torsion.
Geodesics without a particular parameterization are described by a projective connection.
Computational methodsEdit
Efficient solvers for the minimal geodesic problem on surfaces posed as Eikonal equations can be found in ^{[3]}^{[4]}
ApplicationsEdit
This section needs expansion. You can help by adding to it. (June 2014) 
Geodesics serve as the basis to calculate:
 geodesic airframes; see geodesic airframe or geodetic airframe
 geodesic structures – for example geodesic domes
 horizontal distances on or near Earth; see Earth geodesics
 mapping images on surfaces, for rendering; see UV mapping
 robot motion planning (e.g., when painting car parts); see Shortest path problem
See alsoEdit
ReferencesEdit
 ^ "geodesic – definition of geodesic in English from the Oxford dictionary". OxfordDictionaries.com. Retrieved 20160120.
 ^ "Geodesic". MerriamWebster Dictionary.
 ^ R. Kimmel, A. Amir, and A. M. Bruckstein. Finding shortest paths on surfaces using level sets propagation. IEEE Transactions on Pattern Analysis and Machine Intelligence, 17(6):635–640, 1995.
 ^ R. Kimmel and J. A. Sethian. Computing Geodesic Paths on Manifolds in the Proceedings of National Academy of Sciences, 95(15):8431–8435, July, 1998.
 Spivak, Michael (1999), A Comprehensive introduction to differential geometry (Volume 2), Houston, TX: Publish or Perish, ISBN 9780914098713
Wikimedia Commons has media related to Geodesic (mathematics). 
Further readingEdit
This article includes a list of references, but its sources remain unclear because it has insufficient inline citations. (July 2014) (Learn how and when to remove this template message) 
 Adler, Ronald; Bazin, Maurice; Schiffer, Menahem (1975), Introduction to General Relativity (2nd ed.), New York: McGrawHill, ISBN 9780070004238. See chapter 2.
 Abraham, Ralph H.; Marsden, Jerrold E. (1978), Foundations of mechanics, London: BenjaminCummings, ISBN 9780805301021. See section 2.7.
 Jost, Jürgen (2002), Riemannian Geometry and Geometric Analysis, Berlin, New York: SpringerVerlag, ISBN 9783540426271. See section 1.4.
 Kobayashi, Shoshichi; Nomizu, Katsumi (1996), Foundations of Differential Geometry, Vol. 1 (New ed.), WileyInterscience, ISBN 0471157333.
 Landau, L. D.; Lifshitz, E. M. (1975), Classical Theory of Fields, Oxford: Pergamon, ISBN 9780080181769. See section 87.
 Misner, Charles W.; Thorne, Kip; Wheeler, John Archibald (1973), Gravitation, W. H. Freeman, ISBN 9780716703440
 Ortín, Tomás (2004), Gravity and strings, Cambridge University Press, ISBN 9780521824750. Note especially pages 7 and 10.
 Volkov, Yu.A. (2001) [1994], "Geodesic line", in Hazewinkel, Michiel (ed.), Encyclopedia of Mathematics, Springer Science+Business Media B.V. / Kluwer Academic Publishers, ISBN 9781556080104.
 Weinberg, Steven (1972), Gravitation and Cosmology: Principles and Applications of the General Theory of Relativity, New York: John Wiley & Sons, ISBN 9780471925675. See chapter 3.
External linksEdit
 Geodesics Revisited — Introduction to geodesics including two ways of derivation of the equation of geodesic with applications in geometry (geodesic on a sphere and on a torus), mechanics (brachistochrone) and optics (light beam in inhomogeneous medium).
 Geodesics on a parametric surface  sage interact — Interactive SageMath worksheet to calculate and illustrate geodesics on parametric surfaces.
 Totally geodesic submanifold at the Manifold Atlas