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Probability distributions
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Probability distributions
Topics : Concepts of probability density function (p.d.f.) and cumulative distribution function (c.d.f.) Moments of distributions (mean, variance, skewness) Parent distributions Extreme value distributions Ref. : Wind loading and structural response Lecture 3 Dr. J.D. Holmes, Reeding Univeristy
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Probability distributions
Probability density function : Limiting probability (x 0) that the value of a random variable X lies between x and (x + x) Denoted by fX(x) x fX(x) x
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Probability distributions
Probability density function : Probability that X lies between the values a and b is the area under the graph of fX(x) defined by x=a and x=b fX(x) x Pr(a<x<b) x = a b i.e. Since all values of X must fall between - and + : i.e. total area under the graph of fX(x) is equal to 1
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Probability distributions
Cumulative distribution function : The cumulative distribution function (c.d.f.) is the integral between - and x of fX(x) Denoted by FX(x) fX(x) x x = a Fx(a) Area to the left of the x = a line is : FX(a) This is the probability that X is less than a
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Probability distributions
Complementary cumulative distribution function : The complementary cumulative distribution function is the integral between x and + of fX(x) Denoted by GX(x) and equal to : 1- FX(x) fX(x) x Gx(b) x = b Area to the right of the x = b line is : GX(b) This is the probability that X is greater than b
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Probability distributions
Moments of a distribution : Mean value fX(x) x x =X The mean value is the first moment of the probability distribution, i.e. the x coordinate of the centroid of the graph of fX(x)
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Probability distributions
Moments of a distribution : Variance The variance, X2, is the second moment of the probability distribution about the mean value It is equivalent to the second moment of area of a cross section about the centroid The standard deviation, X, is the square root of the variance fX(x) x =X x X
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Probability distributions
Moments of a distribution : skewness Positive skewness indicates that the distribution has a long tail on the positive side of the mean Negative skewness indicates that the distribution has a long tail on the negative side of the mean` x fx(x) positive sx negative sx A distribution that is symmetrical about the mean value has zero skewness
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Probability distributions
Gaussian (normal) distribution : p.d.f. fX(x) x 0.1 0.2 0.3 0.4 -4 -3 -2 -1 1 2 3 4 allows all values of x : -<x< + bell-shaped distribution, zero skewness
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Probability distributions
Gaussian (normal) distribution : c.d.f. FX(x) = ( ) is the cumulative distribution function of a normally distributed variable with mean of zero and unit standard deviation (tabulated in textbooks on probability and statistics) (u) = Used for turbulent velocity fluctuations about the mean wind speed, dynamic structural response, but not for pressure fluctuations or scalar wind speed
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Probability distributions
Lognormal distribution : p.d.f. A random variable, X, whose natural logarithm has a normal distribution, has a Lognormal distribution (m, are the mean and standard deviation of logex) Since logarithms of negative values do not exist, X > 0 the mean value of X is equal to m exp (2/2) the variance of X is equal to m2 exp(2) [exp(2) -1] the skewness of X is equal to [exp(2) + 2][exp(2) - 1]1/2 (positive) Used in structural reliability, and hurricane modeling (e.g. central pressure)
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Probability distributions
Weibull distribution : p.d.f. fX(x) = complementary c.d.f. FX(x) = c.d.f. FX(x) = c = scale parameter (same units as X) k= shape parameter (dimensionless) X must be positive, but no upper limit. Weibull distribution widely used for wind speeds, and sometimes for pressure coefficients
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Probability distributions
Weibull distribution : k=3 k=2 k=1 x 0.0 0.2 0.4 0.6 0.8 1.0 1.2 1 2 3 4 fx(x) Special cases : k=1 Exponential distribution k=2 Rayleigh distribution
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Probability distributions
Poisson distribution : Previous distributions used for continuous random variables (X can take any value over a defined range) Poisson distribution applies to positive integer variables Examples : number of hurricanes occurring in a defined area in a given time number of exceedences of a defined pressure level on a building Probability function : pX(x) = is the mean value of X. Standard deviation = 1/2 is the mean rate of ocurrence per unit time. T is the reference time period
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Probability distributions
Extreme Value distributions : Previous distributions used for all values of a random variables, X - known as ‘parent distributions In many cases in civil engineering we are interested in the largest values, or extremes, of a population for design purposes Examples : flood heights, wind speeds Let Y be the maximum of n independent random variables, X1, X2, …….Xn c.d.f of Y : FY(y) = FX1(y). FX2(y). ……….FXn(y) Special case - all Xi have the same c.d.f : FY(y) = [FX1(y)]n
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Probability distributions
Generalized Extreme Value distribution (G.E.V.) : c.d.f FY(y) = k is the shape factor; a is the scale factor; u is the location parameter Special cases : Type I (k=0) Gumbel exp[exp(-(y-u)/a)] Type II (k<0) Frechet Type III (k>0) ‘Reverse Weibull’ G.E.V (or Types I, II, III separately) - used for extreme wind speeds and pressure coefficients
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Probability distributions
Generalized Extreme Value distribution (G.E.V.) : -6 -4 -2 2 4 6 8 -3 -1 1 3 Reduced variate : -ln[-ln(FY(y)] (y-u)/a Type I k = 0 Type III k = +0.2 Type II k = -0.2 (In this way of plotting, Type I appears as a straight line) Type I, II : Y is unlimited as c.d.f. reduces Type III: Y has an upper limit (may be better for variables with an expected physical upper limit such as wind speeds)
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Probability distributions
Generalized Pareto distribution (G.P.D.) : c.d.f FX(x) = k is the shape factor is the scale factor p.d.f. fX(x) = k = 0 or k<0 : < X < k>0 : < X< (/k) i.e. upper limit G.P.D. is appropriate distribution for independent observations of excesses over defined thresholds e.g. thunderstorm downburst of 70 knots. Excess over 40 knots is 30 knots
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Probability distributions
Generalized Pareto distribution : fx(x) x/ k=+0.5 k=-0.5 G.P.D. can be used with Poisson distribution of storm occurrences to predict extreme winds from storms of a particular type
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