2019
DOI: 10.48550/arxiv.1911.11996
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Existence and uniqueness of global Koopman eigenfunctions for stable fixed points and periodic orbits

Abstract: We consider C 1 dynamical systems having a globally attracting hyperbolic fixed point or periodic orbit and prove existence and uniqueness results for C k,α loc globally defined linearizing semiconjugacies, of which Koopman eigenfunctions are a special case. Our main results both generalize and sharpen Sternberg's C k linearization theorem for hyperbolic sinks, and in particular our corollaries include uniqueness statements for Sternberg linearizations and Floquet normal forms. Additional corollaries include e… Show more

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Cited by 5 publications
(16 citation statements)
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“…where g j (θ) are Floquet eigenfunctions associated with the periodic orbit x γ (θ), and ψ j are isostable coordinates. These isostable coordinates can be defined as level sets of particular eigenfunctions of the Koopman operator [15], [11]. For the most slowly decaying isostable coordinates, an alternative definition can be given that considers the infinite-time decay of initial conditions to the limit cycle [27], [22].…”
Section: Phase-amplitude Reduction Methods and Isostable Coordinatesmentioning
confidence: 99%
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“…where g j (θ) are Floquet eigenfunctions associated with the periodic orbit x γ (θ), and ψ j are isostable coordinates. These isostable coordinates can be defined as level sets of particular eigenfunctions of the Koopman operator [15], [11]. For the most slowly decaying isostable coordinates, an alternative definition can be given that considers the infinite-time decay of initial conditions to the limit cycle [27], [22].…”
Section: Phase-amplitude Reduction Methods and Isostable Coordinatesmentioning
confidence: 99%
“…To implement the adaptive phase-amplitude reduction framework, suppose that ( 9) has a nominal parameter set p 0 that describes the dynamics of an underlying model. It is then possible to rewrite (9) as ẋ = F (x, p) + U e (t, p, x), (11) with the extended input U e (t, p, x) ≡ U (t) + F (x, p 0 ) − F (x, p). Intuitively, the term F (x, p) represents dynamics of the model when using parameter set p, and U e captures both the externally applied input and the mismatch caused when considering the parameter set p as compared to the parameter set p 0 of the underlying model (9).…”
Section: Derivation Of An Adaptive Phase-amplitude Reduction Strategymentioning
confidence: 99%
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“…Proposition 4 Consider the time-varying system (2) with an equilibrium x ⋆ at the origin, 6 and assuming the system is contracting with a time-invariant metric M (x), then there exists a Koopman mapping φ(x, t) satisfying ( 15) and (16).…”
Section: B Extension To Time-varying Systemsmentioning
confidence: 99%
“…The definition (3) is closely aligned with the one given in [22], however, other definitions that compute Fourier averages of observables [20], [21] can also be used. As a point of emphasis, the constructive definition of isostable coordinates (3) is only possible for a subset of eigenvalues with the smallest magnitude real components [29]. Isostable coordinates associated with larger magnitude eigenvalues must be defined implicitly as level sets of Koopman eigenfunctions with decay rates that are governed by their associated λ j .…”
Section: Background: Isostable Reductionmentioning
confidence: 99%