2011
DOI: 10.3923/jas.2011.2154.2162
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Classical and Bayesian Estimations on the Kumaraswamy Distribution using Grouped and Un-grouped Data under Difference Loss Functions

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Cited by 12 publications
(12 citation statements)
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“…Grag [3] derived the distribution of single order statistics, the joint distribution of two order statistics and the distribution of the product and the quotient of two order statistics when the random variables are independent and identically Kum-distributed. Golizadeh et al [4] obtained non-Bayesian and Bayesian estimation for the parameters of the Kum distribution. Moreover, non-Bayesian and Bayesian approaches are used to obtain point and interval estimation of the shape parameters, the reliability and the hazard rate functions of the Kum distribution based on generalized order statistics [5].…”
Section: Original Research Articlementioning
confidence: 99%
“…Grag [3] derived the distribution of single order statistics, the joint distribution of two order statistics and the distribution of the product and the quotient of two order statistics when the random variables are independent and identically Kum-distributed. Golizadeh et al [4] obtained non-Bayesian and Bayesian estimation for the parameters of the Kum distribution. Moreover, non-Bayesian and Bayesian approaches are used to obtain point and interval estimation of the shape parameters, the reliability and the hazard rate functions of the Kum distribution based on generalized order statistics [5].…”
Section: Original Research Articlementioning
confidence: 99%
“…However, it has a closed-form cumulative distribution function which is invertible and for which the moments do exist. The KumD method was widely applied for testing natural phenomena such as test scores, temperatures and daily hydrological data of rain fall, [9][10][11][12]. After that, Abd Al-Fattah [13] derived the inversion of KumD by using the transformation ; KumD (α ,β ) [8].…”
Section: Inverted Kumaraswamy Distributionmentioning
confidence: 99%
“…The distribution is appropriate to natural phenomena whose outcomes are bounded from both sides, such as the individuals' heights, test scores, temperatures and hydrological daily data of rain fall (for more details, see Kumaraswamy [6], Jones [7], Golizadeh et al [8], Sindhu et al [9] and Sharaf El-Deen et al [10]). …”
Section: Introductionmentioning
confidence: 99%