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Geodesic as Limit of Geodesics on PL-Surfaces

机译:测地线作为PL表面上测地线的极限

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We study the problem of convergence of geodesics on PL-surfaces and in particular on subdivision surfaces. More precisely, if a sequence (T_n)_(n∈N) of PL-surfaces converges in distance and in normals to a smooth surface S and if C_n is a geodesic of T_n (i.e. it is locally a shortest path) such that (C_n)_(n∈N) converges to a curve C, we wonder if C is a geodesic of 5. Hildebrandt et al. [11] have already shown that if Cn is a shortest path, then C is a shortest path. In this paper, we provide a counter example showing that this result is false for geodesies. We give a result of convergence for geodesies with additional assumptions concerning the rate of convergence of the normals and of the lengths of the edges. Finally, we apply this result to different subdivisions surfaces (such as Catmull-Clark) assuming that geodesies avoid extraordinary vertices.
机译:我们研究了PL面上,尤其是细分面上的测地线收敛问题。更准确地说,如果PL表面的序列(T_n)_(n∈N)在距离和法线上收敛到光滑表面S,并且C_n是T_n的测地线(即局部为最短路径),则( C_n)_(n∈N)收敛到曲线C,我们想知道C是否为5的测地线。Hildebrandt等人。文献[11]已经表明,如果Cn是最短路径,则C是最短路径。在本文中,我们提供了一个反例,表明该结果对于大地测量学是错误的。我们给出了大地测量的收敛结果,并附加了有关法线和边长的收敛速度的假设。最后,假设测地线避免出现异常顶点,我们将此结果应用于不同的细分曲面(例如Catmull-Clark)。

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