Closed geodesic explained

In differential geometry and dynamical systems, a closed geodesic on a Riemannian manifold is a geodesic that returns to its starting point with the same tangent direction. It may be formalized as the projection of a closed orbit of the geodesic flow on the tangent space of the manifold.

Definition

In a Riemannian manifold (M,g), a closed geodesic is a curve

\gamma:R → M

that is a geodesic for the metric g and is periodic.

Closed geodesics can be characterized by means of a variational principle. Denoting by

ΛM

the space of smooth 1-periodic curves on M, closed geodesics of period 1 are precisely the critical points of the energy function

E:ΛMR

, defined by
1
E(\gamma)=\int
0

g\gamma(t)(

\gamma(t),\gamma(t))dt.

If

\gamma

is a closed geodesic of period p, the reparametrized curve

t\mapsto\gamma(pt)

is a closed geodesic of period 1, and therefore it is a critical point of E. If

\gamma

is a critical point of E, so are the reparametrized curves

\gammam

, for each

m\inN

, defined by

\gammam(t):=\gamma(mt)

. Thus every closed geodesic on M gives rise to an infinite sequence of critical points of the energy E.

Examples

Sn\subsetRn+1

with the standard round Riemannian metric, every great circle is an example of a closed geodesic. Thus, on the sphere, all geodesics are closed. On a smooth surface topologically equivalent to the sphere, this may not be true, but there are always at least three simple closed geodesics; this is the theorem of the three geodesics. Manifolds all of whose geodesics are closed have been thoroughly investigated in the mathematical literature. On a compact hyperbolic surface, whose fundamental group has no torsion, closed geodesics are in one-to-one correspondence with non-trivial conjugacy classes of elements in the Fuchsian group of the surface.

See also

References

"Manifolds all of whose geodesics are closed", Ergebisse Grenzgeb. Math., no. 93, Springer, Berlin, 1978.