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using ''t''<sub>1</sub> = ''εt'' and valid for ''εt'' = O(1). This agrees with the nonlinear [[frequency]] changes found by employing the [[Lindstedt–Poincaré method]].
Higher-order solutions – using the method of multiple scales – require the introduction of additional slow scales, ''i.e.'': ''t''<sub>2</sub> = ''ε''<sup>2</sup> ''t'', ''t''<sub>3</sub> = ''ε''<sup>3</sup> ''t'', etc. However, this introduces possible ambiguities in the perturbation series solution, which require a careful treatment (see {{harvnb|Kevorkian|Cole|1996}}; {{harvnb|Bender|Orszag|1999}}).<ref>Bender & Orszag (1999) p. 551.</ref>
Alternatively, modern sound approaches derive these sorts of models using coordinate transforms ===Coordinate transform to amplitude/phase variables===
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transforms Duffing's equation into the pair that the radius is constant <math>dr/dt=0</math> and the phase evolves according to
:<math>\frac{d\theta}{dt}=1 +\frac38\varepsilon r^2 -\frac{15}{256}\varepsilon^2r^4 +\mathcal O(\varepsilon^3).</math>
That is, Duffing's oscillations are constant amplitude but a different frequencies depending upon the amplitude.<ref>{{citation |first=A.J. |last=Roberts |title=Modelling emergent dynamics in complex systems |url=http://www.maths.adelaide.edu.au/anthony.roberts/modelling.php |accessdate=2013-10-03 }}</ref>
More difficult examples are better treated using a time dependent coordinate transform involving complex exponentials (as also invoked in the previous multiple time scale approach). A web service will perform the analysis for a wide range of examples. <ref>A. J. Roberts, <em>Construct centre manifolds of ordinary or delay differential equations (autonomous)</em> [http://www.maths.adelaide.edu.au/anthony.roberts/gencm.php]</ref>▼
▲More difficult examples are better treated using a time dependent coordinate transform involving complex exponentials (as also invoked in the previous multiple time scale approach). A web service will perform the analysis for a wide range of examples.
==See also==
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