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Fréchet distribution

Continuous probability distribution From Wikipedia, the free encyclopedia

Fréchet distribution
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The Fréchet distribution, also known as inverse Weibull distribution,[2][3] is a special case of the generalized extreme value distribution. It has the cumulative distribution function

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where α > 0 is a shape parameter. It can be generalised to include a location parameter m (the minimum) and a scale parameter s > 0 with the cumulative distribution function

Named for Maurice Fréchet who wrote a related paper in 1927,[4] further work was done by Fisher and Tippett in 1928 and by Gumbel in 1958.[5][6]

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Characteristics

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The single parameter Fréchet, with parameter has standardized moment

(with ) defined only for

where is the Gamma function.

In particular:

  • For the expectation is
  • For the variance is

The quantile of order can be expressed through the inverse of the distribution,

.

In particular the median is:

The mode of the distribution is

Especially for the 3-parameter Fréchet, the first quartile is and the third quartile

Also the quantiles for the mean and mode are:

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Properties

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The cumulative distribution function of the Frechet distribution solves the maximum stability postulate equation.

Scaling relations include:

  • If (continuous uniform distribution) then
  • If then its reciprocal is Weibull-distributed:
  • If then
  • If and then
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Applications

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Fitted cumulative Fréchet distribution to extreme one-day rainfalls
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Fitted decline curve analysis. Duong model can be thought of as a generalization of the Frechet distribution.
  • In hydrology, the Fréchet distribution is applied to extreme events such as annually maximum one-day rainfalls and river discharges.[7] This picture illustrates an example of fitting the Fréchet distribution to ranked annually maximum one-day rainfalls in Oman showing also the 90% confidence belt based on the binomial distribution. The cumulative frequencies of the rainfall data are represented by plotting positions as part of the cumulative frequency analysis. However, in most hydrological applications, the distribution fitting is via the generalized extreme value distribution as this avoids imposing the assumption that the distribution does not have a lower bound (as required by the Frechet distribution). [citation needed]
  • In decline curve analysis, a declining pattern the time series data of oil or gas production rate over time for a well can be described by the Fréchet distribution.[8]
  • One test to assess whether a multivariate distribution is asymptotically dependent or independent consists of transforming the data into standard Fréchet margins using the transformation and then mapping from Cartesian to pseudo-polar coordinates . Values of correspond to the extreme data for which at least one component is large while approximately 1 or 0 corresponds to only one component being extreme.
  • In economics it is used to model the idiosyncratic component of preferences of individuals for different products (Industrial Organization), locations (Urban Economics), or firms (Labor Economics).
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See also

References

Further reading

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