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Lyapunov time
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{{Short description|Timescale of dynamical systems}} In [[mathematics]], the '''Lyapunov time''' is the characteristic timescale on which a [[dynamical system]] is [[chaos theory|chaotic]]. It is named after the [[Russia]]n [[mathematician]] [[Aleksandr Lyapunov]]. It is defined as the inverse of a system's largest [[Lyapunov exponent]].<ref>{{cite book |first1=Boris P. |last1=Bezruchko |first2=Dmitry A. |last2=Smirnov |url=https://books.google.com/books?id=li6JDAEACAAJ |isbn=9783642126000 |publisher=Springer |pages=56–57 |title=Extracting Knowledge from Time Series: An Introduction to Nonlinear Empirical Modeling |date=5 September 2010 }}</ref> ==Use== The Lyapunov time mirrors the limits of the [[predictability]] of the system. By convention, it is defined as the time for the distance between nearby trajectories of the system to increase by a factor of ''[[e (mathematical constant)|e]]''. However, measures in terms of 2-foldings and 10-foldings are sometimes found, since they correspond to the loss of one bit of information or one digit of precision respectively.<ref name="gaspard" /><ref>{{cite arXiv |eprint=1706.08638 |last1=Friedland |first1=G. |last2=Metere |first2=A. |title=Isomorphism between Maximum Lyapunov Exponent and Shannon's Channel Capacity |year=2018 |class=cond-mat.stat-mech }}</ref> While it is used in many applications of dynamical systems theory, it has been particularly used in [[celestial mechanics]] where it is important for the problem of the [[stability of the Solar System]]. However, empirical estimation of the Lyapunov time is often associated with computational or inherent uncertainties.<ref>{{cite journal |doi=10.1086/318732|title=A Comparison Between Methods to Compute Lyapunov Exponents|year=2001|last1=Tancredi|first1=G.|last2=Sánchez|first2=A.|last3=Roig|first3=F.|journal=The Astronomical Journal|volume=121|issue=2|pages=1171–1179|bibcode=2001AJ....121.1171T|doi-access=free}}</ref><ref>{{cite arXiv |eprint=0901.4871 |last1=Gerlach |first1=E. |title=On the Numerical Computability of Asteroidal Lyapunov Times |year=2009 |class=physics.comp-ph }}</ref> ==Examples== Typical values are:<ref name="gaspard">Pierre Gaspard, ''Chaos, Scattering and Statistical Mechanics'', Cambridge University Press, 2005. p. 7</ref> {| class="wikitable" |- ! System !! Lyapunov time |- | [[Pluto]]'s orbit|| 20 million years |- | [[Solar System]] || 5 million years |- | [[Axial tilt]] of [[Mars]] || 1–5 million years |- | Orbit of [[36 Atalante]] || 4,000 years |- | Rotation of [[Hyperion (moon)|Hyperion]] || 36 days |- | Chemical chaotic oscillations || 5.4 minutes |- | [[Hydrodynamic]] chaotic oscillations || 2 seconds |- | 1 cm<sup>3</sup> of [[argon]] at room temperature || 3.7×10<sup>−11</sup> seconds |- | 1 cm<sup>3</sup> of argon at triple point (84 K, 69 kPa) || 3.7×10<sup>−16</sup> seconds |} ==See also== * [[Belousov–Zhabotinsky reaction]] * [[Molecular chaos]] * [[Three-body problem]] ==References== {{reflist}} [[Category:Dynamical systems]]
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