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Closed geodesic : ウィキペディア英語版
Closed geodesic
In differential geometry and dynamical systems, a closed geodesic on a Riemannian manifold is a geodesic that forms a simple closed curve. 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:\mathbb R\rightarrow 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 \Lambda M the space of smooth 1-periodic curves on ''M'', closed geodesics of period 1 are precisely the critical points of the energy function E:\Lambda M\rightarrow\mathbb R, defined by
E(\gamma)=\int_0^1 g_(\dot\gamma(t),\dot\gamma(t))\,\mathrmt.
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 \gamma^m, for each m\in\mathbb N, defined by \gamma^m(t):=\gamma(mt). Thus every closed geodesic on ''M'' gives rise to an infinite sequence of critical points of the energy ''E''.

抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
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