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Introduction to the Modeling and Analysis of Complex Systems

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154 CHAPTER 9. CHAOS2.52.01.51.00.50.00.50 20 40 60 80 100Figure 9.1: Example <strong>of</strong> chaotic behavior, generated using Eq. (8.37) with r = 1.8 <strong>and</strong><strong>the</strong> initial condition x 0 = 0.1.• is a prevalent phenomenon that can be found everywhere in nature, as well asin social <strong>and</strong> engineered environments.The sensitivity <strong>of</strong> chaotic systems <strong>to</strong> initial conditions is particularly well known under<strong>the</strong> moniker <strong>of</strong> <strong>the</strong> “butterfly effect,” which is a metaphorical illustration <strong>of</strong> <strong>the</strong> chaoticnature <strong>of</strong> <strong>the</strong> wea<strong>the</strong>r system in which “a flap <strong>of</strong> a butterfly’s wings in Brazil could se<strong>to</strong>ff a <strong>to</strong>rnado in Texas.” The meaning <strong>of</strong> this expression is that, in a chaotic system,a small perturbation could eventually cause very large-scale difference in <strong>the</strong> long run.Figure 9.2 shows two simulation runs <strong>of</strong> Eq. (8.37) with r = 1.8 <strong>and</strong> two slightly differentinitial conditions, x 0 = 0.1 <strong>and</strong> x 0 = 0.100001. The two simulations are fairly similarfor <strong>the</strong> first several steps, because <strong>the</strong> system is fully deterministic (this is why wea<strong>the</strong>rforecasts for just a few days work pretty well). But <strong>the</strong> “flap <strong>of</strong> <strong>the</strong> butterfly’s wings” (<strong>the</strong>0.000001 difference) grows eventually so big that it separates <strong>the</strong> long-term fates <strong>of</strong> <strong>the</strong>two simulation runs. Such extreme sensitivity <strong>of</strong> chaotic systems makes it practicallyimpossible for us <strong>to</strong> predict exactly <strong>the</strong>ir long-term behaviors (this is why <strong>the</strong>re are notwo-month wea<strong>the</strong>r forecasts 1 ).1 But this doesn’t necessarily mean we can’t predict climate change over longer time scales. What is notpossible with a chaotic system is <strong>the</strong> prediction <strong>of</strong> <strong>the</strong> exact long-term behavior, e.g., when, where, <strong>and</strong> howmuch it will rain over <strong>the</strong> next 12 months. It is possible, though, <strong>to</strong> model <strong>and</strong> predict long-term changes<strong>of</strong> a system’s statistical properties, e.g., <strong>the</strong> average temperature <strong>of</strong> <strong>the</strong> global climate, because it can bedescribed well in a much simpler, non-chaotic model. We shouldn’t use chaos as an excuse <strong>to</strong> avoid making

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