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
that is a
geodesic for the metric
g and is periodic.
Closed geodesics can be characterized by means of a variational principle. Denoting by
the space of smooth 1-periodic curves on
M, closed geodesics of period 1 are precisely the
critical points of the energy function
, defined by
If
is a closed geodesic of period
p, the reparametrized curve
is a closed geodesic of period 1, and therefore it is a critical point of
E. If
is a critical point of
E, so are the reparametrized curves
, for each
, defined by
. Thus every closed geodesic on
M gives rise to an infinite sequence of critical points of the energy
E.
Examples
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.