A simple proof of Gevrey estimates for expansions of quasi-periodic orbits: dissipative models and lower dimensional tori

Abstract

We consider standard-like/Froeschl\'e maps with a dissipation and nonlinear perturbation. That is \[ T(p,q) = ( (1 - γ 3) p + μ + V'(q), q + (1 - γ 3) p + μ + V'(q) 2 π ) \] where p ∈ RD, q ∈ 2 π TD are the dynamical variables. The μ ∈ RD, γ∈ R are parameters of the model. We assume that the potential V is a trigonometric polynomial. Note that when γ 0, the perturbation parameter creates dissipation, which has a drastic effect on the existence of quasi-periodic orbits, hence it is a singular perturbation. We fix a frequency ω ∈ RD and study the existence of quasiperiodic orbits. When there is dissipation, having a quasiperiodic orbit of frequency ω requires adjusting the parameter μ, called the drift. We first study the Lindstedt series (formal power series in ) for quasiperidic orbits with D independent frequencies and the drift when γ 0. We show that, when ω is irrational, the series exist to all orders, and when ω is Diophantine, we show that the formal Lindstedt series are Gevrey. We also study the case when D = 2, but the quasi-periodic orbits have only one independent frequency (Lower dimensional tori). Both when γ = 0 and when γ 0, we show that, under some mild non-degeneracy conditions on V, there are (at least two) formal Lindstedt series defined to all orders and that they are Gevrey. Furthermore, we can take μ along a 1 dimensional space.

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