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When the cdf of ''Y'' is the converse of the Gumbel standard cumulative distribution, <math>P(Y \leq y) = 1 - F(y)</math>, then ''Y'' has a density function that is a ]:<ref> |
When the cdf of ''Y'' is the converse of the Gumbel standard cumulative distribution, <math>P(Y \leq y) = 1 - F(y)</math>, then ''Y'' has a density function that is a ]:<ref>{{Cite journal|doi=10.1016/j.insmatheco.2006.07.003|title=Rational reconstruction of frailty-based mortality models by a generalisation of Gompertz' law of mortality|year=2007|last1=Willemse|first1=W.J.|last2=Kaas|first2=R.|journal=Insurance: Mathematics and Economics|volume=40|issue=3|pages=468}}</ref> however, ''Y'' does not have a ] since the Gompertz distribution is restricted to positive values while ''Y'' can take both positive and negative values. | ||
Theory related to the ] provides a multivariate version of the Gumbel distribution. | Theory related to the ] provides a multivariate version of the Gumbel distribution. | ||
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] with ] of a cumulative Gumbel distribution to maximum one-day October rainfalls.]] | ] with ] of a cumulative Gumbel distribution to maximum one-day October rainfalls.]] | ||
Gumbel has shown that the maximum value (or last ]) in a sample of a ] following an ] approaches the Gumbel distribution closer with increasing sample size.<ref>Gumbel |
Gumbel has shown that the maximum value (or last ]) in a sample of a ] following an ] approaches the Gumbel distribution closer with increasing sample size.<ref>{{cite book|last=Gumbel|first= E. J. |year=1954|asin=B0007DSHG4| title=Statistical theory of extreme values and some practical applications|series=Applied Mathematics Series|volume= 33|edition=1st|url=http://books.google.com/books/about/Statistical_theory_of_extreme_values_and.html?id=SNpJAAAAMAAJ|lccn=QA 1 .U58 no.33|publisher= U.S. Department of Commerce, National Bureau of Standards}}</ref> | ||
In ], therefore, the Gumbel distribution is used to analyze such variables as monthly and annual maximum values of daily rainfall and river discharge volumes,<ref>{{cite book|last=Ritzema |
In ], therefore, the Gumbel distribution is used to analyze such variables as monthly and annual maximum values of daily rainfall and river discharge volumes,<ref>{{cite book|editor-last=Ritzema |editor-first=first=H. P.|first1=R. J.|last1=Oosterbaan|chapter=Chapter 6 Frequency and Regression Analysis|year=1994|title= Drainage Principles and Applications, Publication 16|publisher= International Institute for Land Reclamation and Improvement (ILRI)|location= Wageningen, The Netherlands|pages=175–224|url=http://www.waterlog.info/pdf/freqtxt.pdf|isbn=90-70754-33-9}}</ref> and also to describe droughts.<ref>{{cite journal|doi=10.1016/j.jhydrol.2010.04.035|title=An extreme value analysis of UK drought and projections of change in the future|year=2010|last1=Burke|first1=Eleanor J.|last2=Perry|first2=Richard H.J.|last3=Brown|first3=Simon J.|journal=Journal of Hydrology|volume=388|pages=131}}</ref> | ||
Gumbel has also shown that the ] <big>''r'' / (''n''+1)</big> for the probability of an event - where <big>''r''</big> is the rank number of the observed value in the data series and <big>''n''</big> is the total number of observations - is an ] of the ] around the ] of the distribution. Therefore, this estimator is often used as a ]. | Gumbel has also shown that the ] <big>''r'' / (''n''+1)</big> for the probability of an event - where <big>''r''</big> is the rank number of the observed value in the data series and <big>''n''</big> is the total number of observations - is an ] of the ] around the ] of the distribution. Therefore, this estimator is often used as a ]. | ||
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The blue picture illustrates an example of fitting the Gumbel distribution to ranked maximum one-day October rainfalls showing also the 90% ] based on the ]. The rainfall data are represented by the ] ''r'' / (''n''+1) as part of the ]. | The blue picture illustrates an example of fitting the Gumbel distribution to ranked maximum one-day October rainfalls showing also the 90% ] based on the ]. The rainfall data are represented by the ] ''r'' / (''n''+1) as part of the ]. | ||
In ], the Gumbel distribution approximates the number of terms in a ]<ref>{{cite |
In ], the Gumbel distribution approximates the number of terms in a ]<ref>{{cite journal|doi=10.1215/S0012-7094-41-00826-8|title=Of a positive integer|year=1941|last1=Erdös|first1=Paul|last2=Lehner|first2=Joseph|journal=Duke Mathematical Journal|volume=8|issue=2|pages=335}}</ref> as well as the trend-adjusted sizes of record ] and record gaps between ].<ref>{{cite journal|arxiv=1301.2242|last=Kourbatov|first= A.|title=Maximal gaps between prime k-tuples: a statistical approach|journal=Journal of Integer Sequences|volume= 16 |year=2013}} Article 13.5.2.</ref> | ||
==See also== | ==See also== |
Revision as of 04:01, 23 October 2013
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Cumulative distribution function | |||
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location (real) scale (real) | ||
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where | |||
CDF | |||
Mean | |||
Median | |||
Mode | |||
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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 (a term that is alternatively 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
This section includes a list of references, related reading, or external links, but its sources remain unclear because it lacks inline citations. Please help improve this section by introducing more precise citations. (February 2012) (Learn how and when to remove this message) |
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.
In number theory, the Gumbel distribution approximates the number of terms in a partition of an integer as well as the trend-adjusted sizes of record prime gaps and record gaps between prime constellations.
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.; Kaas, R. (2007). "Rational reconstruction of frailty-based mortality models by a generalisation of Gompertz' law of mortality". Insurance: Mathematics and Economics. 40 (3): 468. doi:10.1016/j.insmatheco.2006.07.003.
- Gumbel, E. J. (1954). Statistical theory of extreme values and some practical applications. Applied Mathematics Series. Vol. 33 (1st ed.). U.S. Department of Commerce, National Bureau of Standards. ASIN B0007DSHG4. LCCN 1 .U58 no.33 QA 1 .U58 no.33.
{{cite book}}
: Check|lccn=
value (help) - Oosterbaan, R. J. (1994). "Chapter 6 Frequency and Regression Analysis". In Ritzema, first=H. P. (ed.). Drainage Principles and Applications, Publication 16 (PDF). Wageningen, The Netherlands: International Institute for Land Reclamation and Improvement (ILRI). pp. 175–224. ISBN 90-70754-33-9.
{{cite book}}
: Missing pipe in:|editor-first=
(help) - Burke, Eleanor J.; Perry, Richard H.J.; Brown, Simon J. (2010). "An extreme value analysis of UK drought and projections of change in the future". Journal of Hydrology. 388: 131. doi:10.1016/j.jhydrol.2010.04.035.
- Erdös, Paul; Lehner, Joseph (1941). "Of a positive integer". Duke Mathematical Journal. 8 (2): 335. doi:10.1215/S0012-7094-41-00826-8.
- Kourbatov, A. (2013). "Maximal gaps between prime k-tuples: a statistical approach". Journal of Integer Sequences. 16. arXiv:1301.2242. Article 13.5.2.