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A Probability Distribution and Its Uses in Fitting Data

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202RAMBERG, TADIKAMALLA, DUDEWICZ AND MYKYTKA2724021I.-> 18COal 150L 120Z 9LdILi3- Z Pi 1 1I I I I I I0.0 0.01 0.02 0.03 0.04 0.05COEFFICIENT OF FRICTION0.06 0.07FIGURE 1. Coefficient of friction relative frequency histogram <strong>and</strong> the fitted distribution.centile (or quantile) function, if the percentile functionexists. The percentile function is simply the <strong>in</strong>verseof the distribution function. This concept isparticularly useful <strong>in</strong> Monte Carlo simulation studiesbecause of the follow<strong>in</strong>g result: If X is a cont<strong>in</strong>uousr<strong>and</strong>om variable with percentile function R, <strong>and</strong> U isa uniform r<strong>and</strong>om variable on the <strong>in</strong>terval zero toone, then the transformation X = R(U) yields a r<strong>and</strong>omvariable with the percentile function R.A specific example is Tukey's [16] lambda functionR(p) = [p - (l - p)X]/ (O?< p ?l1), (1)which is def<strong>in</strong>ed for all nonzero lambda values. (As X-- 0, the logistic distribution results.) Van Dyke [17]compared a normalized version of this function withStudent's t distribution. Filliben [5] used this distributionto approximate symmetric distributions with awide range of tail weights for study<strong>in</strong>g location estimationproblems of symmetric distributions. He alsogave a very complete discussion of the properties ofthe percentile function. Jo<strong>in</strong>er <strong>and</strong> Rosenblatt [7]studied the lambda distribution further <strong>and</strong> gave resultson the sample range. Ramberg <strong>and</strong> Schmeiser[9] showed how this distribution could be used toapproximate many of the well-known symmetric distributions<strong>and</strong> explored its application to MonteCarlo simulation studies.Ramberg <strong>and</strong> Schmeiser [10] generalized (1) to afour-parameter distribution def<strong>in</strong>ed by the percentilefunctionR(p) = A + [pa - (1 - p4]/A2 (0 < p < 1), (2)where X, is a location parameter, ,A is a scale parameter<strong>and</strong> A3 <strong>and</strong> A4 are shape parameters. This distribution,which <strong>in</strong>cludes the orig<strong>in</strong>al lambda distribution,also permits skewed curves to be represented. Althoughthe distribution function does not exist <strong>in</strong>"simple closed form," this should not be of concernto practitioners s<strong>in</strong>ce the same is true of the normaldistribution (whose percentiles are not nearly so easilycomputed). Another asymmetric generalization of(1) was considered by Ramberg [11].The density function correspond<strong>in</strong>g to (2) is givenby:f(x) = f[R(p)]- X2[X3pX3-1 + X4(1 -p)4-1]-i(0O

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