We use cookies to distinguish you from other users and to provide you with a better experience on our websites. Close this message to accept cookies or find out how to manage your cookie settings.
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 .
To save content items to your Kindle, first ensure no-reply@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.
We define and study graphs associated to hexagon decompositions of surfaces by curves and arcs. One of the variants is shown to be quasi-isometric to the pants graph, whereas the other variant is quasi-isometric to (a Cayley graph of) the mapping class group.
Given a surface $\Sigma$ equipped with a set P of marked points, we consider the triangulations of $\Sigma$ with vertex set P. The flip-graph of $\Sigma$ is the graph whose vertices are these triangulations, and whose edges correspond to flipping arcs in these triangulations. The flip-graph of a surface appears in the study of moduli spaces and mapping class groups. We consider the number of geodesics in the flip-graph of $\Sigma$ between two triangulations as a function of their distance. We show that this number grows exponentially provided the surface has enough topology, and that in the remaining cases the growth is polynomial.
In this note we show that the expected value of the separating systole of a random surface of genus g with respect to Weil–Petersson volume behaves like $2\log g $ as the genus goes to infinity. This is in strong contrast to the behavior of the expected value of the systole which, by results of Mirzakhani and Petri, is independent of genus.
Our main point of focus is the set of closed geodesics on hyperbolic surfaces. For any fixed integer k, we are interested in the set of all closed geodesics with at least k (but possibly more) self-intersections. Among these, we consider those of minimal length and investigate their self-intersection numbers. We prove that their intersection numbers are upper bounded by a universal linear function in k (which holds for any hyperbolic surface). Moreover, in the presence of cusps, we get bounds which imply that the self-intersection numbers behave asymptotically like k for growing k.
It is a theorem of Bers that any closed hyperbolic surface admits a pants decomposition consisting of curves of bounded length where the bound only depends on the topology of the surface. The question of the quantification of the optimal constants has been well studied, and the best upper bounds to date are linear in genus, due to a theorem of Buser and Seppälä. The goal of this note is to give a short proof of a linear upper bound that slightly improves the best known bound.
Starting with a classical conjecture of Frobenius on solutions of the Markoff cubic, we are led, via the work of Harvey Cohn, to explore the multiplicities of lengths of simple geodesics on surfaces. We indicate recent progress on this and related questions stemming from the work of Schmutz Schaller. As an illustration we compare the cases of multiplicities on euclidean and hyperbolic once-punctured tori; in the euclidean case basic number theory gives a complete understanding of the spectrum. We explain an elementary construction using iterated Dehn twists that gives useful information about the lengths of simple geodesics in the hyperbolic case. In particular it shows that the marked simple length spectrum satisfies a rigidity condition: knowing just the order in the marked simple length spectrum is enough to determine the surface up to isometry. These results are special cases of a more general result [MP].
Introduction
The length spectrum of a hyperbolic surface is defined as the set of lengths of closed geodesics counted with multiplicities, and has been studied extensively in its relationship with the Laplace operator of a surface. A natural subset of the length spectrum is the simple length spectrum: the set of lengths of simple closed geodesics counted with multiplicities. This set is more naturally related to Teichmüller space and the mapping class group.
Recommend this
Email your librarian or administrator to recommend adding this to your organisation's collection.