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Generalized extreme value distribution

Family of probability distributions

Generalized extreme value distribution

Family of probability distributions

\sigma 0 (scale) \xi \in \mathbb{R} (shape) x \in (-\infty, \infty) when \xi = 0 x \in \big(-\infty, \mu - \tfrac{\sigma}{\xi}\big] when \xi where t(x) = \begin{cases} \left[ 1 + \xi \left( \tfrac{x - \mu}{\sigma} \right) \right]^{-1/\xi} & \text{if } \xi \neq 0 \ \exp\left(-\tfrac{x - \mu}{\sigma} \right) & \text{if } \xi = 0 \end{cases} \mu + \sigma\gamma & \text{if } \xi = 0 \ \infty & \text{if } \xi \geq 1 \end{cases} where g_k = \Gamma(1 - k\xi) (see Gamma function) and \gamma is Euler’s constant \mu - \sigma \ln\ln2 & \text{if } \xi = 0 \end{cases} \mu & \text{if } \xi = 0 \end{cases} \sigma^2 , \frac{\pi^2}{6} & \text{if } \xi = 0 \ \infty & \text{if } \xi \geq \tfrac{1}{2} \end{cases} \dfrac{12 \sqrt{6} , \zeta(3)}{\pi^3} & \text{if } \xi = 0 \end{cases} where \sgn(x) is the sign function and \zeta(x) is the Riemann zeta function \tfrac{12}{5} & \text{if } \xi = 0\end{cases}

In probability theory and statistics, the generalized extreme value (GEV) distribution |access-date=2021-08-06 is a family of continuous probability distributions developed within extreme value theory to combine the Gumbel, Fréchet and Weibull families also known as type I, II and III extreme value distributions. By the extreme value theorem the GEV distribution is the only possible limit distribution of properly normalized maxima of a sequence of independent and identically distributed random variables. Note that a limit distribution needs to exist, which requires regularity conditions on the tail of the distribution. Despite this, the GEV distribution is often used as an approximation to model the maxima of long (finite) sequences of random variables.

In some fields of application the generalized extreme value distribution is known as the Fisher–Tippett distribution, named after R.A. Fisher and L.H.C. Tippett who recognised three different forms outlined below. However usage of this name is sometimes restricted to mean the special case of the Gumbel distribution. The origin of the common functional form for all three distributions dates back to at least , though allegedly it could also have been given by .

Specification

Using the standardized variable s = \tfrac{x - \mu}{\sigma}, where \mu, the location parameter, can be any real number, and \sigma 0 is the scale parameter; the cumulative distribution function of the GEV distribution is then

: F(s; \xi) = \begin{cases} \exp (-\mathrm{e}^{-s}) & \text{for } \xi = 0 , \ \exp \bigl( ! - ( 1 + \xi s)^{-1/\xi} \bigr) & \text{for } \xi \neq 0 \text{ and } \xi s -1 , \ 0 & \text{for } \xi 0 \text{ and } s \le -\tfrac{1}{\xi} , \ 1 & \text{for } \xi

where \xi, the shape parameter, can be any real number. Thus, for \xi 0, the expression is valid for s -\tfrac{1}{\xi}, while for \xi it is valid for s . In the first case, -\tfrac{1}{\xi} is the negative, lower end-point, where F is 0; in the second case, -\tfrac{1}{\xi} is the positive, upper end-point, where F is 1. For \xi = 0, the second expression is formally undefined and is replaced with the first expression, which is the result of taking the limit of the second, as \xi \to 0 in which case s can be any real number.

In the special case of x = \mu, we have s = 0, so F(0; \xi) = \mathrm{e}^{-1} \approx 0.368 regardless of the values of \xi and \sigma.

The probability density function of the standardized distribution is

:f(s; \xi) = \begin{cases} \mathrm{e}^{-s} \exp (-\mathrm{e}^{-s} ) & \text{for } \xi = 0 , \ (1 + \xi s)^{-( 1 + 1/\xi )} \exp\bigl(! -( 1 + \xi s )^{-1/\xi} \bigr) & \text{for } \xi \neq 0 \text{ and } \xi s -1 , \ 0 & \text{otherwise;} \end{cases}

again valid for s -\tfrac{1}{\xi} in the case \xi 0, and for s in the case \xi . The density is zero outside of the relevant range. In the case \xi = 0, the density is positive on the whole real line.

Since the cumulative distribution function is invertible, the quantile function for the GEV distribution has an explicit expression, namely

:Q(p; \mu, \sigma, \xi) = \begin{cases} \mu - \sigma \ln ( -\ln p ) & \text{for } \xi = 0 \text{ and } p \in (0, 1) , \ \mu + \dfrac{\sigma}{\xi} \big( ( -\ln p)^{-\xi} - 1 \big) & \text{for } \xi 0 \text{ and } p \in [0, 1) , \text{ or } \xi

and therefore the quantile density function q = \tfrac{\mathrm{d}Q}{\mathrm{d}p} is

:q(p; \sigma, \xi) = \frac{\sigma}{(-\ln p)^{\xi + 1} ,p} \qquad \text{for } p \in (0, 1) ,

valid for \sigma 0 and for any real \xi.

Example of probability density functions for distributions of the GEV family.

Summary statistics

Using g_k \equiv \Gamma(1 - k\xi) for ~ k \in{1, 2, 3, 4}\ , where \Gamma(\cdot) is the gamma function, some simple statistics of the distribution are given by:

:\operatorname{\mathbb E}( X ) = \mu + (g_1 - 1) , \frac{\sigma}{ \xi } \quad for \xi :\operatorname{Var}( X ) = (g_2 - g_1^2) , \frac{\sigma^2}{\xi^2}\ , :\operatorname{Mode}( X ) = \mu + \bigl(( 1 + \xi )^{-\xi} - 1\bigr) , \frac{\sigma}{ \xi } ~.

The skewness is : \ \operatorname{skewness}( X ) = \begin{cases} \dfrac{g_3 - 3g_2 g_1 + 2g_1^3}{(g_2 - g_1^2)^{3/2} } \cdot \sgn(\xi) & \xi \ne 0\ , \ \dfrac{12\sqrt{6} , \zeta(3)}{\pi^3} \approx 1.14 & \xi = 0 ~. \end{cases}

The excess kurtosis is: :\ \operatorname{kurtosis\ excess}( X ) = \frac{g_4 - 4g_3 g_1 + 6g_2 g_1^2 - 3g_1^4}{(g_2 - g_1^2)^2 } - 3 ~.

Properties

The cumulative distribution function of the generalized extreme value distribution solves the stability postulate equation. The generalized extreme value distribution is a special case of a max-stable distribution, and is a transformation of a min-stable distribution.

Applications

  • The GEV distribution is widely used in the treatment of "tail risks" in fields ranging from insurance to finance. In the latter case, it has been considered as a means of assessing various financial risks via metrics such as value at risk.{{cite report |archive-date = 22 September 2015 |access-date = 17 June 2015 |archive-url = https://web.archive.org/web/20150922161616/http://www.unalmed.edu.co/~ndgirald/Archivos%20Lectura/Archivos%20curso%20Riesgo%20Operativo/moscadelli%202004.pdf |url-status = dead
Fitted GEV probability distribution to monthly maximum one-day rainfalls in October, Surinam
  • However, the resulting shape parameters have been found to lie in the range leading to undefined means and variances, which underlines the fact that reliable data analysis is often impossible.{{cite web |url-status=dead |access-date=4 December 2019 |archive-date=17 April 2023 |archive-url=https://web.archive.org/web/20230417010614/https://citeseerx.ist.psu.edu/viewdoc/download?doi=10.1.1.523.6456&rep=rep1&type=pdf
  • In hydrology the GEV distribution is applied to extreme events such as annual maximum one-day rainfalls and river discharges. The blue picture illustrates an example of fitting the GEV distribution to ranked annually maximum one-day rainfalls showing also the 90% confidence belt based on the binomial distribution. The rainfall data are represented by plotting positions as part of the cumulative frequency analysis.

Prediction

  • It is often of interest to predict probabilities of out-of-sample data under the assumption that both the training data and the out-of-sample data follow a GEV distribution.
  • Predictions of probabilities generated by substituting maximum likelihood estimates of the GEV parameters into the cumulative distribution function ignore parameter uncertainty. As a result, the probabilities are not well calibrated, do not reflect the frequencies of out-of-sample events, and, in particular, underestimate the probabilities of out-of-sample tail events.
  • Predictions generated using the objective Bayesian approach of calibrating prior prediction have been shown to greatly reduce this underestimation, although not completely eliminate it. Calibrating prior prediction is implemented in the R software package fitdistcp.

Example for Normally distributed variables

Let \ \left{\ X_i\ \big|\ 1 \le i \le n\ \right}\ be i.i.d. normally distributed random variables with mean 0 and variance 1. The Fisher–Tippett–Gnedenko theorem tells us that \ \max {\ X_i\ \big|\ 1 \le i \le n\ } \sim GEV(\mu_n, \sigma_n, 0)\ , where

\begin{align} \mu_n &= \Phi^{-1}\left( 1 - \frac{\ 1\ }{ n } \right) \ \sigma_n &= \Phi^{-1}\left( 1 - \frac{ 1 }{\ n\ \mathrm{e}\ } \right)- \Phi^{-1}\left(1-\frac{\ 1\ }{ n } \right) ~. \end{align}

This allow us to estimate e.g. the mean of \ \max {\ X_i\ \big|\ 1 \le i \le n\ }\ from the mean of the GEV distribution:

\begin{align} \operatorname{\mathbb E}\left{\ \max\left{\ X_i\ \big|\ 1 \le i \le n\ \right}\ \right} & \approx \mu_n + \gamma_{\mathsf E}\ \sigma_n \ &= (1 - \gamma_{\mathsf E})\ \Phi^{-1}\left( 1 - \frac{\ 1\ }{ n } \right) + \gamma_{\mathsf E}\ \Phi^{-1}\left( 1 - \frac{1}{\ e\ n\ } \right) \ &= \sqrt{\log \left(\frac{ n^2 }{\ 2 \pi\ \log \left(\frac{n^2}{2\pi} \right)\ }\right) ~}\ \cdot\ \left(1 + \frac{ \gamma }{\ \log n\ } + \mathcal{o} \left(\frac{ 1 }{\ \log n\ } \right) \right)\ , \end{align}

where \ \gamma_{\mathsf E}\ is the Euler–Mascheroni constant.

References

|editor-first=Linda L. |editor-last=Wright

|access-date = 2023-02-27 |archive-date = 2023-03-31 |archive-url = https://web.archive.org/web/20230331230821/http://uryasev.ams.stonybrook.edu/wp-content/uploads/2019/10/Norton2019_CVaR_bPOE.pdf |url-status = dead

References

  1. (2025-02-20). "Reducing reliability bias in assessments of extreme weather risk using calibrating priors". Advances in Statistical Climatology, Meteorology and Oceanography.
  2. Jewson, Stephen. (2025-04-23). "fitdistcp: Distribution Fitting with Calibrating Priors for Commonly Used Distributions". Comprehensive R Archive Network.
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