Revision as of 02:24, 23 July 2013 editWJVaughn3 (talk | contribs)77 edits →Quantile function and Generating Gumbel variates← Previous edit | Revision as of 14:40, 29 July 2013 edit undoWJVaughn3 (talk | contribs)77 editsm Formatting changes onlyNext edit → | ||
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parameters =<math>\mu\!</math> ] (])<br /><math>\beta>0\!</math> ] (real)| | parameters =<math>\mu\!</math> ] (])<br /><math>\beta>0\!</math> ] (real)| | ||
support =<math>x \in (-\infty; +\infty)\!</math>| | support =<math>x \in (-\infty; +\infty)\!</math>| | ||
pdf =<math>\frac{1}{\beta}e^{-z |
pdf =<math>\frac{1}{\beta}e^{-(z+e^{-z})}\!</math><br /> where <math>z=\frac{x-\mu}{\beta}\!</math>| | ||
cdf =<math>e^{-e^{-(x-\mu)/\beta}}\!</math>| | cdf =<math>e^{-e^{-(x-\mu)/\beta}}\!</math>| | ||
mean =<math>\mu + \beta\,\gamma\!</math>| | mean =<math>\mu + \beta\,\gamma\!</math>| | ||
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The mode is μ, while the median is <math>\mu-\beta \ln\left(\ln 2\right),</math> and the mean is given by | The mode is μ, while the median is <math>\mu-\beta \ln\left(\ln 2\right),</math> and the mean is given by | ||
:<math>\operatorname{E}(X)=\mu+\gamma\beta ,</math> | :<math>\operatorname{E}(X)=\mu+\gamma\beta ,</math> | ||
where <math>\gamma</math> = ] <math>\approx |
where <math>\gamma</math> = ] <math>\approx 0.5772.</math> | ||
⚫ | The standard deviation is <math>\beta \pi/\sqrt{6}.</math> | ||
⚫ | ==Standard Gumbel distribution== | ||
The standard deviation is | |||
⚫ | The standard Gumbel distribution is the case where <math>\mu = 0</math> and <math>\beta = 1</math> with cumulative distribution function | ||
⚫ | |||
⚫ | |||
⚫ | The standard Gumbel distribution is the case where |
||
:<math>F(x) = e^{-e^{(-x)}}\,</math> | :<math>F(x) = e^{-e^{(-x)}}\,</math> | ||
and probability density function | and probability density function | ||
:<math>f(x) = e^{-x |
:<math>f(x) = e^{-(x+e^{-x})}.</math> | ||
⚫ | In this case mode is 0, the median is <math>-\ln(\ln(2)) \approx</math> |
||
⚫ | In this case the mode is 0, the median is <math>-\ln(\ln(2)) \approx 0.3665</math>, the mean is <math>\gamma</math>, and the standard deviation is <math>\pi/\sqrt{6} \approx 1.2825.</math> | ||
: <math> \pi/\sqrt{6} \approx</math> 1.2825. | |||
==Quantile function and Generating Gumbel variates== | ==Quantile function and Generating Gumbel variates== | ||
Since the quantile function(inverse |
Since the quantile function(inverse ]), <math>Q(p)</math>, of a Gumbel distribution is given by | ||
:<math>Q(p)=\mu+\beta\ln(1/\ln(1/p)),</math> | :<math>Q(p)=\mu+\beta\ln(1/\ln(1/p)),</math> | ||
the variate Q( |
the variate <math>Q(U)</math> has a Gumbel distribution with parameters <math>\mu</math> and <math>\beta</math> when the random variate <math>U</math> is drawn from the ] on the interval <math>(0,1)</math>. | ||
the ] on the interval (0,1). | |||
==Related distributions== | ==Related distributions== |
Revision as of 14:40, 29 July 2013
Probability density function | |||
Cumulative distribution function | |||
Parameters |
location (real) scale (real) | ||
---|---|---|---|
Support | |||
where | |||
CDF | |||
Mean | |||
Median | |||
Mode | |||
Variance | |||
Skewness | |||
Excess kurtosis | |||
Entropy | |||
MGF | |||
CF |
In probability theory and statistics, the Gumbel distribution is used to model the distribution of the maximum (or the minimum) of a number of samples of various distributions. Such a distribution might be used to represent the distribution of the maximum level of a river in a particular year if there was a list of maximum values for the past ten years. It is useful in predicting the chance that an extreme earthquake, flood or other natural disaster will occur.
The potential applicability of the Gumbel distribution to represent the distribution of maxima relates to extreme value theory which indicates that it is likely to be useful if the distribution of the underlying sample data is of the normal or exponential type.
The Gumbel distribution is a particular case of the generalized extreme value distribution (also known as the Fisher-Tippett distribution). It is also known as the log-Weibull distribution and the double exponential distribution (which is sometimes used to refer to the Laplace distribution). It is often incorrectly labelled as Gompertz distribution.
In the latent variable formulation of the multinomial logit model — common in discrete choice theory — the errors of the latent variables follow a Gumbel distribution. This is useful because the difference of two Gumbel-distributed random variables has a logistic distribution.
The Gumbel distribution is named after Emil Julius Gumbel (1891–1966).
Properties
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The cumulative distribution function of the Gumbel distribution is
The mode is μ, while the median is and the mean is given by
where = Euler–Mascheroni constant The standard deviation is
Standard Gumbel distribution
The standard Gumbel distribution is the case where and with cumulative distribution function
and probability density function
In this case the mode is 0, the median is , the mean is , and the standard deviation is
Quantile function and Generating Gumbel variates
Since the quantile function(inverse cumulative distribution function), , of a Gumbel distribution is given by
the variate has a Gumbel distribution with parameters and when the random variate is drawn from the uniform distribution on the interval .
Related distributions
When the cdf of Y is the converse of the Gumbel standard cumulative distribution, , then Y has a density function that is a Gompertz function: however, Y does not have a Gompertz distribution since the Gompertz distribution is restricted to positive values while Y can take both positive and negative values.
Theory related to the generalized multivariate log-gamma distribution provides a multivariate version of the Gumbel distribution.
Graphic paper
In pre-software times graphic paper was used to picture the Gumbel distribution (see illustration). The paper is based on linearization of the cumulative distribution function :
In the paper the horizontal axis is constructed at a double log scale. The vertical axis is linear. By plotting on the horizontal axis of the paper and the -variable on the vertical axis, the distribution is represented by a straight line with a slope 1. When distribution fitting software like CumFreq became available, the task of plotting the distribution was made easier, as is demonstrated in the section below.
Application
Gumbel has shown that the maximum value (or last order statistic) in a sample of a random variable following an exponential distribution approaches the Gumbel distribution closer with increasing sample size.
In hydrology, therefore, the Gumbel distribution is used to analyze such variables as monthly and annual maximum values of daily rainfall and river discharge volumes, and also to describe droughts.
Gumbel has also shown that the estimator r / (n+1) for the probability of an event - where r is the rank number of the observed value in the data series and n is the total number of observations - is an unbiased estimator of the cumulative probability around the mode of the distribution. Therefore, this estimator is often used as a plotting position.
The blue picture illustrates an example of fitting the Gumbel distribution to ranked maximum one-day October rainfalls showing also the 90% confidence belt based on the binomial distribution. The rainfall data are represented by the plotting position r / (n+1) as part of the cumulative frequency analysis.
See also
- Type-1 Gumbel distribution
- Type-2 Gumbel distribution
- Extreme value theory
- Generalized extreme value distribution
- Fisher–Tippett–Gnedenko theorem
External links
References
- Willemse, W. J. and Kaas, R., "Rational reconstruction of frailty-based mortality models by a generalisation of Gompertz’ law of mortality", Insurance: Mathematics and Economics, 40 (3) (2007), 468–484.
- Gumbel, E.J. 1954. "Statistical theory of extreme values and some practical applications". Applied Mathematics Series, 33. U.S. Department of Commerce, National Bureau of Standards.
- Ritzema (ed.), H.P. (1994). Frequency and Regression Analysis (PDF). Chapter 6 in: Drainage Principles and Applications, Publication 16, International Institute for Land Reclamation and Improvement (ILRI), Wageningen, The Netherlands. pp. 175–224. ISBN 90-70754-33-9.
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has generic name (help) - Burke, E.J.; Perry R.H.J.; Brown, S.J. (2010) "An extreme value analysis of UK drought and projections of change in the future", Journal of Hydrology