Gumbel distribution
The Gumbel distribution, also known as the type I extreme value distribution, is a continuous probability distribution that models the limiting distribution of the maximum (or the negative of the minimum) of a large number of independent and identically distributed random variables drawn from distributions in its domain of attraction, such as the exponential, normal, lognormal, or gamma distributions.[1][2] It plays a central role in extreme value theory as one of three asymptotic forms for maxima, specifically the Fisher-Tippett type I, which applies to distributions with exponentially decaying tails.[1][2] The distribution is parameterized by a location parameter μ (real-valued) and a scale parameter β > 0.[1][2] For the maximum case, the probability density function (PDF) is given byf(x; \mu, \beta) = \frac{1}{\beta} \exp\left( -\frac{x - \mu}{\beta} - \exp\left( -\frac{x - \mu}{\beta} \right) \right),
and the cumulative distribution function (CDF) is
F(x; \mu, \beta) = \exp\left( -\exp\left( -\frac{x - \mu}{\beta} \right) \right). [2][1] The minimum case uses a reflected form with PDF
f(x; \mu, \beta) = \frac{1}{\beta} \exp\left( \frac{x - \mu}{\beta} - \exp\left( \frac{x - \mu}{\beta} \right) \right)
and CDF
F(x; \mu, \beta) = 1 - \exp\left( -\exp\left( \frac{x - \mu}{\beta} \right) \right). [2] In the standard form, μ = 0 and β = 1.[2] Notable properties include a mean of μ + γβ for the maximum case, where γ ≈ 0.57721 is the Euler-Mascheroni constant, and a variance of (π²/6)β² ≈ 1.64493β².[1][2] The skewness is positive at approximately 1.13955, and the kurtosis is 5.4 (excess kurtosis of 2.4), reflecting its asymmetric tail toward higher values.[2] The mode is at μ, and the median is μ - β ln(ln 2) ≈ μ + 0.366513β.[2] The distribution is stable under maxima operations, meaning the maximum of independent Gumbel variables follows a shifted and scaled Gumbel distribution.[1] Originally derived by Ronald A. Fisher and Leonard H.C. Tippett in 1928 as part of their classification of extreme value limits, the distribution gained prominence through the applications of Emil J. Gumbel, who first used it systematically for flood frequency analysis in 1941 and detailed its theory in his 1958 book Statistics of Extremes.[1][3] It forms a special case of the generalized extreme value (GEV) distribution when the shape parameter is zero.[2] The Gumbel distribution finds extensive use in fields requiring modeling of rare events, such as hydrology for predicting flood peaks and rainfall extremes, reliability engineering for assessing material strengths and failure times, meteorology for wind speed maxima, and environmental science for analyzing pollutant concentrations.[2][3] In these applications, it enables estimation of return levels for events with specified probabilities, often fitted via methods like probability-weighted moments or maximum likelihood.[2]