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1 Studies in the History of Statistics and Probability ... - Sheynin, Oscar

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smooth<strong>in</strong>g is, however, <strong>in</strong> general less than it is when calculatedaccord<strong>in</strong>g to <strong>the</strong> rules <strong>of</strong> statistics.It occurs because, when decid<strong>in</strong>g by naked eye, we have to do witha given graph, with a result determ<strong>in</strong>ed by r<strong>and</strong>om experiment<strong>in</strong>g; on<strong>the</strong> o<strong>the</strong>r h<strong>and</strong>, when work<strong>in</strong>g by statistical methods, we apply astatistical model <strong>and</strong> <strong>the</strong>refore also cover <strong>the</strong> possible scatter <strong>of</strong> <strong>the</strong>results <strong>of</strong> r<strong>and</strong>om experiments <strong>the</strong>mselves from one <strong>of</strong> <strong>the</strong>irrealizations to ano<strong>the</strong>r one. However, <strong>the</strong> general problem <strong>of</strong> <strong>the</strong> realpossibilities <strong>of</strong> <strong>the</strong> naked eye methods dem<strong>and</strong>s wide experimental<strong>in</strong>vestigation.3. The Theory <strong>of</strong> Stochastic ProcessesHowever beneficial (<strong>in</strong> suitable cases) is <strong>the</strong> method <strong>of</strong> leastsquares, a glance at <strong>the</strong> observational series <strong>of</strong>ten conv<strong>in</strong>ces us that <strong>the</strong>model <strong>of</strong> trend with error can not describe <strong>the</strong> observations, s<strong>in</strong>ce weare unable to isolate by naked eye a determ<strong>in</strong>ate curve withobservational po<strong>in</strong>ts chaotically scattered around it. This is whatSlutsky (1927/1937, p. 105), a co-creator <strong>of</strong> <strong>the</strong> <strong>the</strong>ory <strong>of</strong> stochasticprocesses, wrote about it:Almost all <strong>of</strong> <strong>the</strong> phenomena <strong>of</strong> economic life, like many o<strong>the</strong>rprocesses, social, meteorological, <strong>and</strong> o<strong>the</strong>rs, occur <strong>in</strong> sequences <strong>of</strong>ris<strong>in</strong>g <strong>and</strong> fall<strong>in</strong>g movements, like waves. Just as waves follow<strong>in</strong>g eacho<strong>the</strong>r on <strong>the</strong> sea do not repeat each o<strong>the</strong>r perfectly, so economic cyclesnever repeat earlier ones exactly ei<strong>the</strong>r <strong>in</strong> duration or <strong>in</strong> amplitude.Never<strong>the</strong>less, <strong>in</strong> both cases, it is almost always possible to detect, even<strong>in</strong> <strong>the</strong> multitude <strong>of</strong> <strong>in</strong>dividual peculiarities <strong>of</strong> <strong>the</strong> phenomena, marks <strong>of</strong>certa<strong>in</strong> approximate uniformities <strong>and</strong> regularities. The eye <strong>of</strong> <strong>the</strong>observer <strong>in</strong>st<strong>in</strong>ctively discovers on waves <strong>of</strong> a certa<strong>in</strong> order o<strong>the</strong>rsmaller waves, so that <strong>the</strong> idea <strong>of</strong> harmonic analysis [...] presents itselfto <strong>the</strong> m<strong>in</strong>d almost spontaneously.The idea <strong>of</strong> harmonic analysis can never<strong>the</strong>less attempted to beachieved by <strong>the</strong> model <strong>of</strong> trend with error. It is done by <strong>the</strong> so-calledmethod <strong>of</strong> periodogram that preceded <strong>the</strong> methods <strong>of</strong> <strong>the</strong> <strong>the</strong>ory <strong>of</strong>stochastic processes <strong>and</strong> we will briefly consider it.3.1. The periodogram method. Suppose that our observationsmade at discrete moments <strong>of</strong> time, each second, say, can be describedby <strong>the</strong> modelx t = s<strong>in</strong>(λ 0 t + φ) + δ t , t = 0, 1, ..., n (3.1)where λ 0 is some parameter (circular frequency <strong>of</strong> oscillation), φ, <strong>the</strong>phase <strong>of</strong> oscillation <strong>and</strong> δ i , r<strong>and</strong>om error. Suppose that λ 0 is much lessthan 2π, so that successive observations <strong>of</strong> only one component s<strong>in</strong>(λ 0 t+ φ) would provide a clearly seen s<strong>in</strong>e curve each unit <strong>of</strong> time (whichis much shorter than <strong>the</strong> period <strong>of</strong> oscillation, 2π/λ 0 ). The addition <strong>of</strong>r<strong>and</strong>om errors (suppose, for <strong>the</strong> sake <strong>of</strong> simplicity, <strong>in</strong>dependent) willcerta<strong>in</strong>ly corrupt <strong>the</strong> picture. So how to reconstruct <strong>the</strong> frequency λ 0 ?Multiply our observations x i by s<strong>in</strong>(λt) <strong>and</strong> cos(λt) where λ is avariable, <strong>and</strong> consider <strong>the</strong> sums64

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