Skip to main content Accessibility help
×
Hostname: page-component-7479d7b7d-qs9v7 Total loading time: 0 Render date: 2024-07-13T08:03:07.338Z Has data issue: false hasContentIssue false

7 - The poles and cut loci of a surface of revolution

Published online by Cambridge University Press:  14 August 2009

Katsuhiro Shiohama
Affiliation:
Saga University, Japan
Takashi Shioya
Affiliation:
Tohoku University, Japan
Minoru Tanaka
Affiliation:
Tokai University, Japan
Get access

Summary

It is not easy to find a nontrivial pole even on a surface of revolution, unless the latter has a nonpositive Gaussian curvature. We shall give a necessary and sufficient condition for a surface of revolution to have nontrivial poles. The proof is achieved by obtaining Jacobi fields along any geodesic (see [101]). The method is found in a classical work of von Mangoldt [59]. We will also determine the cut loci of a certain class of surfaces of revolution containing well-known examples: the two-sheeted hyperboloids of revolution and the paraboloids of revolution (see [102]). von Mangoldt proved in [59] that any point on a two-sheeted hyperboloid of revolution is a pole if the point is sufficiently close to the vertex. Furthermore, he proved in [59] that the two umbilic points of a two-sheeted hyperboloid are poles and that the poles of any elliptic paraboloid are the two umbilic points. These surfaces are typical examples of a Liouville surface. A definition of global Liouville surfaces was introduced by Kiyohara in [44]. See also [40] for poles on noncompact complete Liouville surfaces.

Properties of geodesics

A surface of revolution means a complete Riemannian manifold (M, g) homeomorphic to R2 that admits a point p such that the Gaussian curvature of M is constant on S(p, t) for each positive t. The point p is called the vertex of the surface of revolution.

Throughout this chapter (M, g) denotes a surface of revolution and p denotes the vertex of the surface.

Type
Chapter
Information
Publisher: Cambridge University Press
Print publication year: 2003

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

Save book to Kindle

To save this book to your Kindle, first ensure coreplatform@cambridge.org is added to your Approved Personal Document E-mail List under your Personal Document Settings on the Manage Your Content and Devices page of your Amazon account. Then enter the ‘name’ part of your Kindle email address below. Find out more about saving to your Kindle.

Note you can select to save to either the @free.kindle.com or @kindle.com variations. ‘@free.kindle.com’ emails are free but can only be saved to your device when it is connected to wi-fi. ‘@kindle.com’ emails can be delivered even when you are not connected to wi-fi, but note that service fees apply.

Find out more about the Kindle Personal Document Service.

Available formats
×

Save book to Dropbox

To save content items to your account, please confirm that you agree to abide by our usage policies. If this is the first time you use this feature, you will be asked to authorise Cambridge Core to connect with your account. Find out more about saving content to Dropbox.

Available formats
×

Save book to Google Drive

To save content items to your account, please confirm that you agree to abide by our usage policies. If this is the first time you use this feature, you will be asked to authorise Cambridge Core to connect with your account. Find out more about saving content to Google Drive.

Available formats
×