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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 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''.
抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)』 ■ウィキペディアで「closed geodesic」の詳細全文を読む
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