A scientist, discover<strong>in</strong>g someth<strong>in</strong>g remarkable (as <strong>the</strong> Laplaceancentral limit <strong>the</strong>orem) evidently can not keep from apply<strong>in</strong>g iteverywhere. For example, <strong>in</strong> our time Wiener proposed to apply <strong>the</strong><strong>the</strong>ory <strong>of</strong> extrapolation <strong>of</strong> stochastic processes for forecast<strong>in</strong>g <strong>the</strong> route<strong>of</strong> an airplane under anti-aircraft fire. That route however is not astochastic process, or at least not such process for which <strong>the</strong>re exists a<strong>the</strong>ory <strong>of</strong> extrapolation <strong>and</strong> Wiener’s proposal was senseless.Evidently, science is collectively created; true, it is not beyondquestion whe<strong>the</strong>r an essential discovery can be made collectively, or isit necessary to have an outst<strong>and</strong><strong>in</strong>g scientist <strong>in</strong> a collective with itso<strong>the</strong>r members work<strong>in</strong>g <strong>in</strong> essence as his assistants. But what isundoubtedly a collective process is <strong>the</strong> delivery <strong>of</strong> science from <strong>the</strong>rubbish which some scientists usually adduce to <strong>the</strong>ir real discoveries.4.6. When <strong>the</strong> central limit <strong>the</strong>orem can not be applied? That<strong>the</strong>orem is one <strong>of</strong> <strong>the</strong> reasons for believ<strong>in</strong>g that observational resultsusually obey <strong>the</strong> normal distribution. If only <strong>the</strong>y, ξ 1 , ..., ξ n , are known,but not <strong>the</strong> parameters <strong>of</strong> <strong>the</strong> correspond<strong>in</strong>g law, we are able todeterm<strong>in</strong>e <strong>the</strong>m approximately by appropriate methods. Indeed,accord<strong>in</strong>g to <strong>the</strong> law <strong>of</strong> large numbersa = Eξ i ≈ (1/n) (ξ 1 +... + ξ n ) = ξ .It can be shown that1σ ∑ (ξ ξ) .−n2 2 2≈i− = sn 1 i=1The <strong>the</strong>ory <strong>of</strong> errors allows to determ<strong>in</strong>e <strong>the</strong> precision <strong>of</strong> thoseapproximate values.In general, <strong>the</strong> observations are ra<strong>the</strong>r well describable by <strong>the</strong>normal law thus determ<strong>in</strong>ed. In o<strong>the</strong>r words ifF(x) = P{ ξ i < x},N(x, ξ , s) be<strong>in</strong>g those probabilities calculated accord<strong>in</strong>g to <strong>the</strong> normaldistribution, <strong>the</strong>nF(x) ≈ N(x, ξ , s).However, this approximate equality is sometimes very perceptivelyviolated. It happens when <strong>the</strong> values <strong>of</strong> x are such that F(x) is near 0 or1, − that its so-called tail areas are <strong>in</strong>volved.Let us beg<strong>in</strong> by consider<strong>in</strong>g why those areas are practicallysignificant <strong>in</strong> a special way. Suppose we <strong>in</strong>tend to build some tallstructure which will have to withst<strong>and</strong> high w<strong>in</strong>ds (or, if you wish, aspillway which has to pass spr<strong>in</strong>g floods, etc). We desire to reckonwith such w<strong>in</strong>d velocities that happen sufficiently rarely, once <strong>in</strong> acentury, say. But how are we to f<strong>in</strong>d out that velocity? Or, if ξ(t) is thatvelocity at moment t, we ought to <strong>in</strong>dicate such a number x, that42
P{max ξ(t) ≥ x} = 0.01, 0 ≤ t ≤ 1where t is measured <strong>in</strong> years <strong>and</strong> <strong>the</strong> left part <strong>of</strong> <strong>the</strong> <strong>in</strong>equality is <strong>the</strong>maximal yearly w<strong>in</strong>d velocity.Suppose that we know <strong>the</strong> values ξ 1 , ξ 2 , ..., ξ n <strong>of</strong> <strong>the</strong> maximalvelocity dur<strong>in</strong>g <strong>the</strong> first, <strong>the</strong> second, ..., n-th year dur<strong>in</strong>g whichmeteorological observations were made. However, w<strong>in</strong>d velocities hadnot been recorded cont<strong>in</strong>uously but only several times a day, so thatthose maximal yearly velocities are <strong>in</strong> essence unknown. For <strong>the</strong> timebe<strong>in</strong>g, let us never<strong>the</strong>less abstract ourselves from this extremelyessential difficulty.And so, we have those observations <strong>of</strong> <strong>the</strong> r<strong>and</strong>om variable ξ, <strong>the</strong>maximal yearly w<strong>in</strong>d velocity, <strong>and</strong> we wish to assign an x such thatP{ξ ≥ x} = 0.01. (4.11)Had <strong>the</strong> number n been very large, we would have been obliged toselect such an x that about a hundredth part <strong>of</strong> <strong>the</strong> ξ i will be larger thanit. The trouble, however, is that n, <strong>the</strong> number <strong>of</strong> years dur<strong>in</strong>g whichobservations are available, is much less than 100. Then, if x is suchthat (4.11) is fulfilled, that is,P{ξ i ≥ x} = 0.01 for each i,<strong>the</strong> number <strong>of</strong> variables ξ i larger than x will obey <strong>the</strong> Poisson law withparameter λ = 0.01n < 1. It will follow that most likely all <strong>of</strong> our ξ i willbe less than x so that we are only able to say that x should be largerthan each <strong>of</strong> <strong>the</strong> ξ i ′s with no upper boundary available.Therefore, we are tempted to smooth our ξ 1 , ..., ξ n by some law, forexample by <strong>the</strong> normal law N( x; ξ, s ) <strong>and</strong> determ<strong>in</strong>e x from equationN( x; ξ, s ) = 1− 0.01 = 0.99.Or, we will propose to identify <strong>the</strong> tail areas <strong>of</strong> <strong>the</strong> unknown functionF(x) with those <strong>of</strong> <strong>the</strong> normal law.We turn <strong>the</strong> readers’ attention to <strong>the</strong> fact that such a procedureshould not be trusted ei<strong>the</strong>r when apply<strong>in</strong>g <strong>the</strong> normal, or any o<strong>the</strong>rlaw, <strong>and</strong> that <strong>the</strong>re exist both <strong>the</strong>oretical grounds <strong>and</strong> considerationsbased on statistical experiments for that <strong>in</strong>ference. Theoretical groundsconsist <strong>in</strong> that <strong>the</strong> central limit <strong>the</strong>orem only states that <strong>the</strong> difference*between <strong>the</strong> exact distribution function P{ sn< x}<strong>and</strong> <strong>the</strong> normal lawis small:P s x x*{n< } − N( ) → 0.For example, if that probability P = 0.95, N(x) = 0.99 <strong>and</strong> <strong>the</strong>difference is only 0.04 which is sufficiently small. However, <strong>the</strong>relative error*[1 − P{ sn< x}] ÷ [1 − N( x)] = 400%43
- Page 1 and 2: Studies in the History of Statistic
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The verification of the truth of a
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In the purely scientific sense this
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ought to learn at once the simple t
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the material world science had inde
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values of (2.1) realized in the n e
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*several dozen. The totality µ ica
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Mendelian laws. It is not sufficien
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example, the problem of the objecti
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a linear function is not restricted
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258 - 82 - 176 cases or 68.5% of al
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What objections can be made? First,
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Kolman E. (1939 Russian), Perversio
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measurement is provided. Recently,
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which means that sooner or later th
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The foundations of the Mises approa
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A rather subtle arsenal is develope
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4.3. General remarks on §§ 4.1 an
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BibliographyAlimov Yu. I. (1976, 19
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processes are now going on in the s
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obtaining a deviation from the theo
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VIOscar SheyninOn the Bernoulli Law