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In mathematics, a
geodesic is a generalization of the notion of a "Line (mathematics)" to "
manifolds".In presence of a Metric (mathematics), geodesics are defined to be (
locally) the shortest path between points on the space. In the presence of an affine connection, geodesics are defined to be curves whose
tangent vectors remain parallel if they are
parallel transport along it.
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, namely, a
line 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.
Geodesics are of particular importance in general relativity.
Introduction
The shortest path between two points in a curved space can be found by writing the
equation for the length of a curve, and then minimizing this length using standard techniques of
calculus and differential equations. Equivalently, a different quantity may be defined, termed the
energy of the curve; minimizing the energy leads to the same equations for a geodesic. 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.
Geodesics are commonly seen in the study of Riemannian geometry and more generally
metric geometry. In relativistic
physics, geodesics 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 described by geodesics in the theory of general relativity. More generally, the topic of sub-Riemannian 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 manifold and
pseudo-Riemannian manifolds. The article
geodesic (general relativity) discusses the special case of general relativity in greater detail.
Examples
The most familiar examples are the straight lines in
Euclidean geometry.On a
sphere, the geodesics are the
great circles.The shortest path from point
A to point
B on a sphere is given by the shorter piece of the great circle passing through
A and
B. If
A and
B are
antipodal points (like the North pole and the South pole), then there are
infinitely many shortest paths between them.
Metric geometry
In
metric geometry, a geodesic is a curve which is everywhere
locally a distance minimizer. More precisely, a
curve γ:
I →
M from the
unit interval I to the
metric space M is a
geodesic if there is a mathematical constant
v ≥ 0 such that for any
t ∈
I there is a neighborhood
J of
t in
I such that for any
t1,
t2 ∈
J we have
d(\gamma(t_1),\gamma(t_2))=v|t_1-t_2|.\,
This generalizes the notion of geodesic for Riemannian manifolds. However, in metric geometry the geodesic considered is almost always equipped with
Curve#Length of curves, i.e. in the above identity
v = 1 and
d(\gamma(t_1),\gamma(t_2))=|t_1-t_2|.\,
If the last equality is satisfied for all
t1,
t2 ∈
I, the geodesic is called a
minimizing geodesic or
shortest path.
In general, a metric space may have no geodesics, except constant curves.
(Pseudo-)Riemannian geometry
Just as in a standard metric space, a
geodesic on a (pseudo-Riemannian manifold-)
Riemannian manifold M is defined as a curve γ(
t) minimizes the length of the curve. Explicitly, we can write the length of any curve as
l(\gamma)=\int_\gamma \sqrt{ \pm g(\dot\gamma(t),\dot\gamma(t)) }\,dt\ ,
where \dot\gamma represents the derivative with respect to t, and is a vector. The sign in the square root is chosen once for a given curve, to ensure that the square root is a real number. The positive sign is chosen for spacelike curves; in a pseudo-Riemannian manifold, the negative sign may be chosen for timelike curves. A geodesic, then, is the curve which extremizes this quantity (locally).
In the case of a manifold with
torsion of connection-free and metric tensor
connection (mathematics) (which is almost always assumed to be the case in Relativity, for example), a geodesic curve is also an
autoparallel curve. That is, the curve parallel transports its own tangent vector, so
\dot\gamma^\mu \nabla_\mu \dot\gamma^\nu = 0
at each point along the curve. Here, ∇ stands for the Levi-Civita connection on
M.
In this case, using
local coordinates on
M, we can write the
geodesic equation (using the summation convention) as
\frac{d^2x^\lambda }{dt^2} + \Gamma^{\lambda}_{~\mu \nu }\frac{dx^\mu }{dt}\frac{dx^\nu }{dt} = 0\ ,
where x^\mu (t) are the coordinates of the curve γ(
t) and \Gamma^{\lambda }_{~\mu \nu } are the Christoffel symbols. This is just 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.
Geodesics can also be defined as Stationary point curves for the following
action (physics) functional
S(\gamma)=\frac{1}{2}\int g(\dot\gamma(t),\dot\gamma(t))\,dt,
where g is a Riemannian (or pseudo-Riemannian) metric. In pure mathematics, this quantity would generally be referred to as an
energy. The geodesic equation can then be obtained as the
Euler-Lagrange equations of motion for this action.
In a similar manner, one can obtain geodesics as a solution of the Hamilton–Jacobi equations, with (pseudo-)Riemannian metric taken as Hamiltonian mechanics. See
Hamiltonian mechanics#Riemannian manifolds for further details.
Existence and uniqueness
The
local existence and uniqueness theorem for geodesics states that geodesics exist, and are unique; this is a variant of the
Frobenius theorem (differential topology). More precisely:
For any point
p in
M and for any vector
V in
TpM (the tangent space to
M at
p) there exists a unique geodesic \gamma \, :
I →
M such that
:\gamma(0) = p \, and
:\dot\gamma(0) = V,
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
R².The proof of this theorem follows from the theory of ordinary differential equations, by noticing that the geodesic equation is a second-order ODE. Existence and uniqueness then follow from the Picard-Lindelöf theorem for the solutions of ODEs with prescribed initial conditions. γ depends smooth function on both
p and
V.
Geodesic flow
Geodesic flow is an \mathbb R-
group action on
tangent bundle T(M) of a manifold M defined in the following way
G^t(V)=\dot\gamma_V(t)
where t\in \mathbb R, V\in T(M) and \gamma_V denotes the geodesic with initial data \dot\gamma_V(0)=V.
It defines a
Hamiltonian flow on (co)tangent bundle with the (pseudo-)Riemannian metric as the Hamiltonian. In particular it preserves the (pseudo-)Riemannian metric g, i.e.
g(G^t(V),G^t(V))=g(V,V).
That makes possible to define geodesic flow on unit tangent bundle UT(M) of the Riemannian manifold M.
Geodesic spray
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.
Affine and projective geodesics
In the presence of a metric, geodesics are (locally) the length-minimizing curves. However, even if a manifold lacks a metric, geodesics are still well-defined in the presence of an
affine connection. A curve in such a manifold is a geodesic if its tangent vector remains parallel to the curve when it is
parallel transport along it.
See also
References
- Jurgen Jost, Riemannian Geometry and Geometric Analysis, (2002) Springer-Verlag, Berlin ISBN 3-540-42627-2 See section 1.4.
- Ronald Adler, Maurice Bazin, Menahem Schiffer, Introduction to General Relativity (Second Edition), (1975) McGraw-Hill New York, ISBN 0-07-000423-4 See chapter 2.
- Ralph Abraham and Jarrold E. Marsden, Foundations of Mechanics, (1978) Benjamin-Cummings, London ISBN 0-8053-0102-X See section 2.7.
- Steven Weinberg, Gravitation and Cosmology: Principles and Applications of the General Theory of Relativity, (1972) John Wiley & Sons, New York ISBN 0-471-92567-5 See chapter 3.
- Lev D. Landau and Evgenii M. Lifschitz, The Classical Theory of Fields, (1973) Pergammon Press, Oxford ISBN 0-08-018176-7 See section 87.
- Charles W. Misner, Kip S. Thorne, John Archibald Wheeler, Gravitation, (1970) W.H. Freeman, New York; ISBN 0-7167-0344-0.
- Tomás Ortín, Gravity and Strings, (2004) Cambridge University Press, New York. Note especially pages 7 and 10.
External links
- Caltech Tutorial on Relativity — A nice, simple explanation of geodesics with accompanying animation.
- Geomath
In mathematics, a
geodesic is a generalization of the notion of a "Line (mathematics)" to "manifolds".In presence of a Metric (mathematics), geodesics are defined to be (
locally) the shortest path between points on the space. In the presence of an
affine connection, geodesics are defined to be curves whose tangent vectors remain parallel if they are
parallel transport along it.
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, namely, a line 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.
Geodesics are of particular importance in
general relativity.
Introduction
The shortest path between two points in a curved space can be found by writing the
equation for the length of a
curve, and then minimizing this length using standard techniques of calculus and differential equations. Equivalently, a different quantity may be defined, termed the
energy of the curve; minimizing the energy leads to the same equations for a geodesic. 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.
Geodesics are commonly seen in the study of
Riemannian geometry and more generally
metric geometry. In relativistic physics, geodesics 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 described by geodesics in the theory of
general relativity. More generally, the topic of
sub-Riemannian 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 manifold and
pseudo-Riemannian manifolds. The article geodesic (general relativity) discusses the special case of general relativity in greater detail.
Examples
The most familiar examples are the straight lines in
Euclidean geometry.On a
sphere, the geodesics are the
great circles.The shortest path from point
A to point
B on a sphere is given by the shorter piece of the great circle passing through
A and
B. If
A and
B are antipodal points (like the North pole and the South pole), then there are
infinitely many shortest paths between them.
Metric geometry
In
metric geometry, a geodesic is a curve which is everywhere
locally a
distance minimizer. More precisely, a
curve γ:
I →
M from the unit interval
I to the metric space
M is a
geodesic if there is a
mathematical constant v ≥ 0 such that for any
t ∈
I there is a neighborhood
J of
t in
I such that for any
t1,
t2 ∈
J we have
d(\gamma(t_1),\gamma(t_2))=v|t_1-t_2|.\,
This generalizes the notion of geodesic for Riemannian manifolds. However, in metric geometry the geodesic considered is almost always equipped with
Curve#Length of curves, i.e. in the above identity
v = 1 and
d(\gamma(t_1),\gamma(t_2))=|t_1-t_2|.\,
If the last equality is satisfied for all
t1,
t2 ∈
I, the geodesic is called a
minimizing geodesic or
shortest path.
In general, a metric space may have no geodesics, except constant curves.
(Pseudo-)Riemannian geometry
Just as in a standard metric space, a
geodesic on a (
pseudo-Riemannian manifold-)
Riemannian manifold M is defined as a
curve γ(
t) minimizes the length of the curve. Explicitly, we can write the length of any curve as
l(\gamma)=\int_\gamma \sqrt{ \pm g(\dot\gamma(t),\dot\gamma(t)) }\,dt\ ,
where \dot\gamma represents the derivative with respect to t, and is a vector. The sign in the square root is chosen once for a given curve, to ensure that the square root is a real number. The positive sign is chosen for spacelike curves; in a pseudo-Riemannian manifold, the negative sign may be chosen for timelike curves. A geodesic, then, is the curve which extremizes this quantity (locally).
In the case of a manifold with
torsion of connection-free and
metric tensor connection (mathematics) (which is almost always assumed to be the case in Relativity, for example), a geodesic curve is also an
autoparallel curve. That is, the curve parallel transports its own tangent vector, so
\dot\gamma^\mu \nabla_\mu \dot\gamma^\nu = 0
at each point along the curve. Here, ∇ stands for the
Levi-Civita connection on
M.
In this case, using
local coordinates on
M, we can write the
geodesic equation (using the summation convention) as
\frac{d^2x^\lambda }{dt^2} + \Gamma^{\lambda}_{~\mu \nu }\frac{dx^\mu }{dt}\frac{dx^\nu }{dt} = 0\ ,
where x^\mu (t) are the coordinates of the curve γ(
t) and \Gamma^{\lambda }_{~\mu \nu } are the Christoffel symbols. This is just 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.
Geodesics can also be defined as Stationary point curves for the following
action (physics) functional
S(\gamma)=\frac{1}{2}\int g(\dot\gamma(t),\dot\gamma(t))\,dt,
where g is a Riemannian (or pseudo-Riemannian) metric. In pure mathematics, this quantity would generally be referred to as an
energy. The geodesic equation can then be obtained as the Euler-Lagrange equations of motion for this action.
In a similar manner, one can obtain geodesics as a solution of the
Hamilton–Jacobi equations, with (pseudo-)Riemannian metric taken as Hamiltonian mechanics. See
Hamiltonian mechanics#Riemannian manifolds for further details.
Existence and uniqueness
The
local existence and uniqueness theorem for geodesics states that geodesics exist, and are unique; this is a variant of the
Frobenius theorem (differential topology). More precisely:
For any point
p in
M and for any vector
V in
TpM (the
tangent space to
M at
p) there exists a unique geodesic \gamma \, :
I →
M such that
:\gamma(0) = p \, and
:\dot\gamma(0) = V,
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
R².The proof of this theorem follows from the theory of
ordinary differential equations, by noticing that the geodesic equation is a second-order ODE. Existence and uniqueness then follow from the Picard-Lindelöf theorem for the solutions of ODEs with prescribed initial conditions. γ depends
smooth function on both
p and
V.
Geodesic flow
Geodesic flow is an \mathbb R-group action on
tangent bundle T(M) of a manifold M defined in the following way
G^t(V)=\dot\gamma_V(t)
where t\in \mathbb R, V\in T(M) and \gamma_V denotes the geodesic with initial data \dot\gamma_V(0)=V.
It defines a Hamiltonian flow on (co)tangent bundle with the (pseudo-)Riemannian metric as the Hamiltonian. In particular it preserves the (pseudo-)Riemannian metric g, i.e.
g(G^t(V),G^t(V))=g(V,V).
That makes possible to define geodesic flow on
unit tangent bundle UT(M) of the Riemannian manifold M.
Geodesic spray
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.
Affine and projective geodesics
In the presence of a metric, geodesics are (locally) the length-minimizing curves. However, even if a manifold lacks a metric, geodesics are still well-defined in the presence of an
affine connection. A curve in such a manifold is a geodesic if its tangent vector remains parallel to the curve when it is
parallel transport along it.
See also
- Basic introduction to the mathematics of curved spacetime
- Complex geodesic
- Differential geometry of curves
- Exponential map
- Geodesic dome
- Geodesic (general relativity)
- Geodesics as Hamiltonian flows
- Hopf-Rinow theorem
- Intrinsic metric
- Jacobi field
- Quasigeodesic
- Solving the geodesic equations
- Barnes Wallis, who applied geodesics to aircraft structural design in the design of the Vickers Wellesley and Vickers Wellington aircraft, and the R100 airship.
References
- Jurgen Jost, Riemannian Geometry and Geometric Analysis, (2002) Springer-Verlag, Berlin ISBN 3-540-42627-2 See section 1.4.
- Ronald Adler, Maurice Bazin, Menahem Schiffer, Introduction to General Relativity (Second Edition), (1975) McGraw-Hill New York, ISBN 0-07-000423-4 See chapter 2.
- Ralph Abraham and Jarrold E. Marsden, Foundations of Mechanics, (1978) Benjamin-Cummings, London ISBN 0-8053-0102-X See section 2.7.
- Steven Weinberg, Gravitation and Cosmology: Principles and Applications of the General Theory of Relativity, (1972) John Wiley & Sons, New York ISBN 0-471-92567-5 See chapter 3.
- Lev D. Landau and Evgenii M. Lifschitz, The Classical Theory of Fields, (1973) Pergammon Press, Oxford ISBN 0-08-018176-7 See section 87.
- Charles W. Misner, Kip S. Thorne, John Archibald Wheeler, Gravitation, (1970) W.H. Freeman, New York; ISBN 0-7167-0344-0.
- Tomás Ortín, Gravity and Strings, (2004) Cambridge University Press, New York. Note especially pages 7 and 10.
External links
- Caltech Tutorial on Relativity — A nice, simple explanation of geodesics with accompanying animation.
- Geomath
Geodesic - Wikipedia, the free encyclopedia
In mathematics, a geodesic /ˌdʒiəˈdɛsɪk, -ˈdisɪk/ [jee-uh-des-ik, -dee-sik] is a generalization of the notion of a "straight line" to "curved spaces".
Geodesic dome - Wikipedia, the free encyclopedia
A geodesic dome is an almost spherical structure based on a network of great circles (geodesics) lying approximately on the surface of a sphere.
Geodesic -- from Wolfram MathWorld
A geodesic is a locally length-minimizing curve. Equivalently, it is a path that a particle which is not accelerating would follow. In the plane, the geodesics are straight lines.
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