2005
DOI: 10.1590/s0103-97332005000100010
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Simulating a chaotic process

Abstract: Computer simulations of partial differential equations of mathematical physics typically lead to some kind of high-dimensional dynamical system. When there is chaotic behavior we are faced with fundamental dynamical difficulties. We choose as a paradigm of such high-dimensional system a kicked double rotor. This system is investigated for parameter values at which it is strongly non-hyperbolic through a mechanism called unstable dimension variability, through which there are periodic orbits embedded in a chaot… Show more

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Cited by 4 publications
(5 citation statements)
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“…The selection of augmenting the nonlinear volatility models with chaos theory is based on the following. Chaotic behavior means high sensitivity to initial conditions (Viana and Barbosa 2005). Small differences in initial conditions give important outcomes in chaotic behavior, since very small differentiation in initial conditions (Wernecke et al 2017) leads to enormous differences between expected and realized values in the long term.…”
Section: Introductionmentioning
confidence: 99%
“…The selection of augmenting the nonlinear volatility models with chaos theory is based on the following. Chaotic behavior means high sensitivity to initial conditions (Viana and Barbosa 2005). Small differences in initial conditions give important outcomes in chaotic behavior, since very small differentiation in initial conditions (Wernecke et al 2017) leads to enormous differences between expected and realized values in the long term.…”
Section: Introductionmentioning
confidence: 99%
“…The UDV is reflected and quantified by the fluctuations around zero of the finite-time exponent closest to zero (Davidchack & Lai 2000;Viana et al 2005). These fluctuations around the zero value of the finite-time exponents are then a good indicator of the non-hyperbolic nature of the orbit.…”
Section: Analysis Of the Resultsmentioning
confidence: 99%
“…If f were globally hyperbolic, then a shadowing trajectory exists for all time, which has zero mismatch, and the gradient descent algorithm will converge to such a trajectory if the observational noise is sufficiently small [28]. This cannot be said of a non-hyperbolic system [8,21,22,31]. Of course, if a non-hyperbolic system happens to be locally hyperbolic in the region of x and y, then some of the results pertaining to (globally) hyperbolic systems may apply, but this does not help when the system is non-hyperbolic in this region.…”
Section: Resultsmentioning
confidence: 99%
“…The author, for example, has applied GDI to a simple quasi-geostrophic model of the atmosphere [18] (dimension ≈ 1500) and an operational weather forecasting model at reduced resolution [15] (dimension ≈ 7.5 × 10 5 ). In both of these applications the model certainly has Lyapunov exponents near zero, and possibly local Lyapunov exponents that fluctuate about zero [8,21,22,31]. Three important issues that arise in the application of GDI are:…”
Section: Applications and Discussionmentioning
confidence: 99%
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