<strong>the</strong> structural function <strong>of</strong> <strong>the</strong> contents <strong>of</strong> <strong>the</strong> useful component is <strong>of</strong> <strong>the</strong>typeD(r) = αlnr + βwhere r is <strong>the</strong> distance between sample po<strong>in</strong>ts <strong>and</strong> α <strong>and</strong> β, parametersdeterm<strong>in</strong>ed by observation. However, <strong>the</strong> book has a number <strong>of</strong><strong>in</strong>consistencies. Thus, <strong>the</strong> logarithmic dependence is cont<strong>in</strong>ued <strong>in</strong>to <strong>the</strong><strong>in</strong>terval <strong>of</strong> small values <strong>of</strong> r which is impossible because D(r) is a nonnegativemagnitude. Then, <strong>in</strong> some cases <strong>the</strong> subject concerns <strong>the</strong>content, <strong>in</strong> o<strong>the</strong>r <strong>in</strong>stances, its logarithm. In addition, no statisticalchecks are made. But still, <strong>the</strong> factual material impresses so stronglythat careful reliable studies <strong>in</strong> <strong>the</strong> same direction become desirable.In radio physics, <strong>the</strong> scientific level is high <strong>and</strong> similar<strong>in</strong>consistencies just can not occur. However, as far as we know, noreports about successful apply<strong>in</strong>g <strong>the</strong> model <strong>of</strong> process with stationary<strong>in</strong>crements are <strong>in</strong> existence. Rytov (1966) only formulated ahypo<strong>the</strong>sis that <strong>the</strong> phenomenon <strong>of</strong> flicker should be thus described.In conclud<strong>in</strong>g, I deal <strong>in</strong> more detail with <strong>the</strong> statistical <strong>the</strong>ory <strong>of</strong>turbulence <strong>and</strong> <strong>the</strong> problem <strong>of</strong> forecast<strong>in</strong>g.3.6. Statistical <strong>the</strong>ory <strong>of</strong> turbulence. This <strong>the</strong>ory provides abrilliant success <strong>of</strong> a purely statistical description <strong>of</strong> a phenomenon, <strong>of</strong>a highly developed <strong>and</strong> very complicated turbulence with a largenumber <strong>of</strong> vortical movements on differ<strong>in</strong>g scales. Kolmogorov <strong>and</strong>Obukhov founded <strong>the</strong> basis <strong>of</strong> <strong>the</strong> <strong>the</strong>ory before 1941. Experimentalconfirmation <strong>of</strong> <strong>the</strong>ir <strong>the</strong>oretical conclusions dem<strong>and</strong>ed perfectmeasur<strong>in</strong>g <strong>in</strong>struments <strong>and</strong> up to 25 years. Application <strong>of</strong> that <strong>the</strong>oryto problems <strong>in</strong> propagation <strong>of</strong> electromagnetic <strong>and</strong> acousticoscillations <strong>in</strong> <strong>the</strong> atmosphere is also be<strong>in</strong>g developed.A precise knowledge <strong>of</strong> <strong>the</strong> field <strong>of</strong> velocities <strong>in</strong> a turbulent currentis underst<strong>and</strong>ably both impossible <strong>and</strong> useless. Indeed, had we somemethod <strong>of</strong> calculat<strong>in</strong>g all <strong>the</strong> velocities at all po<strong>in</strong>ts, <strong>the</strong>ir registrationwith sufficient precision would have alone dem<strong>and</strong>ed an unimag<strong>in</strong>ableamount <strong>of</strong> paper or magnetic tape <strong>and</strong> work with so much <strong>in</strong>formationis absolutely impossible. The situation should be resolved by someversion <strong>of</strong> a statistical description.It occurred that <strong>the</strong> ma<strong>in</strong> suitable notions can be borrowed from <strong>the</strong>correlation <strong>the</strong>ory; however, <strong>in</strong> <strong>the</strong>ir <strong>in</strong>itial form <strong>the</strong>y were <strong>in</strong>sufficient.There is a scientific law stat<strong>in</strong>g that ex nihilo nihil fit which means thatan application <strong>of</strong> established <strong>the</strong>ories does not cover anyth<strong>in</strong>g new.Without go<strong>in</strong>g <strong>in</strong>to ma<strong>the</strong>matical detail, I will attempt to showexactly how does this law work <strong>in</strong> case <strong>of</strong> turbulence <strong>and</strong> what newconsiderations it was necessary to draw for gett<strong>in</strong>g <strong>the</strong> th<strong>in</strong>gs mov<strong>in</strong>g.Imag<strong>in</strong>e a turbulent current. Its mean velocity depends on concreteconditions (what <strong>and</strong> where is <strong>the</strong> current set <strong>in</strong>to motion [...]) <strong>and</strong> it issenseless to describe it by statistical methods. However, <strong>the</strong>differences <strong>of</strong> velocity <strong>in</strong> various po<strong>in</strong>ts <strong>of</strong> <strong>the</strong> current <strong>and</strong> <strong>in</strong> differ<strong>in</strong>gmoments <strong>of</strong> time less depend on <strong>in</strong>itial conditions <strong>and</strong> to a largerextent are determ<strong>in</strong>ed by <strong>the</strong> properties <strong>of</strong> <strong>the</strong> liquid or gas itself. So,let us study <strong>the</strong> differences78
u(x 1 , x 2 , t 1 , t 2 ) = v(x 1 , t 1 ) − v(x 2 , t 2 )where v(x, t) is <strong>the</strong> velocity <strong>of</strong> <strong>the</strong> liquid at po<strong>in</strong>t x <strong>and</strong> moment t with<strong>the</strong> po<strong>in</strong>t x be<strong>in</strong>g remote from <strong>the</strong> boundaries <strong>of</strong> <strong>the</strong> current <strong>and</strong> tsufficiently large for <strong>the</strong> stationary condition to be established.It is natural to suppose that <strong>the</strong> turbulence is stationary <strong>in</strong> <strong>the</strong> sensethat <strong>the</strong> statistical characteristics <strong>of</strong> <strong>the</strong> difference u only depend on <strong>the</strong>difference t 1 − t 2 = τ. The three-dimensional variables x 1 , x 2 as also <strong>the</strong>difference u itself, that is, a three-dimensional vector, still rema<strong>in</strong>. Wehave a three-dimensional field <strong>of</strong> vectors depend<strong>in</strong>g on six space <strong>and</strong>two temporal variables. Its statistical properties however only dependon <strong>the</strong> difference between <strong>the</strong> latter. If stopp<strong>in</strong>g here <strong>and</strong> expect<strong>in</strong>g todeterm<strong>in</strong>e experimentally <strong>the</strong> statistical characteristics <strong>of</strong> such a field,<strong>the</strong> experiment will <strong>in</strong>variably fail: it is practically impossible <strong>and</strong>science f<strong>in</strong>ds itself <strong>in</strong> a cul-de-sac.And this is exactly <strong>the</strong> situation <strong>in</strong> some o<strong>the</strong>r sciences. R<strong>and</strong>omstress tensors, r<strong>and</strong>om strength, elasticity etc can be <strong>in</strong>troduced but <strong>the</strong>advantage <strong>of</strong> <strong>the</strong>se notions is zero s<strong>in</strong>ce <strong>the</strong>ir statistical characteristicscan not be determ<strong>in</strong>ed. Fur<strong>the</strong>r <strong>the</strong>oretical development <strong>of</strong> <strong>the</strong> <strong>the</strong>ory<strong>of</strong> turbulence was necessary, o<strong>the</strong>rwise no science would haveemerged <strong>the</strong>re.First <strong>of</strong> all, <strong>in</strong> a sufficiently developed turbulence all po<strong>in</strong>ts <strong>and</strong> alldirections should have <strong>the</strong> same rights. This statement seems simplebut actually is ra<strong>the</strong>r subtle. Indeed, we can imag<strong>in</strong>e a measur<strong>in</strong>gdevice consist<strong>in</strong>g <strong>of</strong> three vectors (x, e 1 , e 2 ) <strong>the</strong> last two <strong>of</strong> <strong>the</strong>mapplied to <strong>the</strong> beg<strong>in</strong>n<strong>in</strong>g <strong>of</strong> vector x <strong>and</strong> all three fixed toge<strong>the</strong>r. Anobservation consists <strong>in</strong> apply<strong>in</strong>g <strong>the</strong> beg<strong>in</strong>n<strong>in</strong>g <strong>of</strong> vector x to po<strong>in</strong>t x 1<strong>of</strong> <strong>the</strong> current so that its end will be at po<strong>in</strong>t x 2 = x 1 + x <strong>and</strong> weconstruct <strong>the</strong> projection <strong>of</strong> <strong>the</strong> difference <strong>of</strong> velocitys v(x 2 , t) − v(x 1 , t)on directions e 1 <strong>and</strong> e 2 which will be two r<strong>and</strong>om variables. Incorrelation <strong>the</strong>ory, <strong>the</strong>ir correlation is considered observable. Thiscorrelation should not change when <strong>the</strong> triplet (x, e 1 , e 2 ) is rotatedanyhow as a solid body nor should it depend on po<strong>in</strong>t x 1 . Turbulencesatisfy<strong>in</strong>g this condition is called locally isotropic.It can be shown that, given such turbulence <strong>and</strong> an <strong>in</strong>compressibleliquid, all <strong>the</strong> statistical characteristics <strong>of</strong> <strong>the</strong> vector field u(x 1 , x 2 , t 1 , t 2 )are expressed through characteristics <strong>of</strong> any <strong>of</strong> its components, i. e., <strong>of</strong><strong>the</strong> projection <strong>of</strong> that field on any coord<strong>in</strong>ate axis. We may consider x 1<strong>and</strong> x 2 situated on that axis <strong>and</strong> so <strong>the</strong> problem is reduced to oner<strong>and</strong>om function <strong>of</strong> two one-dimensional space <strong>and</strong> two temporalvariables.The reduction to one k<strong>in</strong>d <strong>of</strong> variables, ei<strong>the</strong>r space or temporal, ispossible due to <strong>the</strong> hypo<strong>the</strong>sis <strong>of</strong> freez<strong>in</strong>g which means that <strong>the</strong>turbulent curls are carried along <strong>the</strong> ma<strong>in</strong> current without change, asthough <strong>the</strong>y were frozen <strong>in</strong> <strong>the</strong> liquid. In such cases we do not have tomeasure turbulence <strong>in</strong> various po<strong>in</strong>ts x 1 <strong>and</strong> x 2 . We arrange <strong>the</strong> l<strong>in</strong>e (x 1 ,x 2 ) along <strong>the</strong> velocity <strong>of</strong> <strong>the</strong> ma<strong>in</strong> current, put our measur<strong>in</strong>g device atpo<strong>in</strong>t x 2 <strong>and</strong> wait for <strong>the</strong> turbulence to move from x 1 to x 2 . Thus, all isreduced to temporal functions only. This hypo<strong>the</strong>sis (strictly speak<strong>in</strong>g,its statistical characteristics ra<strong>the</strong>r than <strong>the</strong> turbulence itself) waschecked experimentally <strong>and</strong> fit well enough.79
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Studies in the History of Statistic
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Introduction by CompilerI am presen
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(Lect. Notes Math., No. 1021, 1983,
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sufficiently securely that a carefu
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is energy?) from chapter 4 of Feynm
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demand to apply transfinite numbers
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for stating that Ω consists of ele
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chances to draw a more suitable apa
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Let the space of elementary events
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2.3. Independence. When desiring to
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Eξ = ∑ aipi.Our form of definiti
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absolutely precisely if the pertine
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where x is any real number. If dens
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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