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Escape of mass and entropy for geodesic flows

Published online by Cambridge University Press:  28 June 2017

FELIPE RIQUELME and
ANIBAL VELOZO
FELIPE RIQUELME
Affiliation:
IMA, Pontificia Universidad Católica de Valparaíso, Blanco Viel 596, Cerro Barón, Valparaíso, Chile email friquelme.math@gmail.com
ANIBAL VELOZO
Affiliation:
Princeton University, Princeton, NJ 08544-1000, USA email avelozo@math.princeton.edu
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Abstract

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In this paper, we study the ergodic theory of the geodesic flow on negatively curved geometrically finite manifolds. We prove that the measure-theoretical entropy is upper semicontinuous when there is no loss of mass. In the case where mass is lost, the critical exponents of parabolic subgroups of the fundamental group have a significant meaning. More precisely, the failure of upper-semicontinuity of the entropy is determined by the maximal parabolic critical exponent. We also study the pressure of positive Hölder-continuous potentials going to zero through the cusps. We prove that the pressure map $t\mapsto P(tF)$ is differentiable until it undergoes a phase transition, after which it becomes constant. This description allows us, in particular, to compute the entropy of the geodesic flow at infinity.

Information

Type
Original Article
Information
Ergodic Theory and Dynamical Systems , Volume 39 , Issue 2 , February 2019, pp. 446 - 473
Copyright
© Cambridge University Press, 2017 

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