Fréchet distribution

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Fréchet
Probability density function
PDF of the Fréchet distribution
Cumulative distribution function
CDF of the Fréchet distribution
Parameters shape.
(Optionally, two more parameters)
scale (default: )
location of minimum (default: )
Support
PDF
CDF
Mean
Median
Mode
Variance
Skewness
Excess kurtosis
Entropy
, where is the
Euler–Mascheroni constant.
MGF [1] Note: Moment exists if
CF [1]

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

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

Fisher and Tippett in 1928 and by Gumbel in 1958.[5][6]

Characteristics

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:

Applications

Fitted cumulative Fréchet distribution to extreme one-day rainfalls

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]

Fitted decline curve analysis. Duong model can be thought of as a generalization of the Frechet distribution.
  • 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 (
    Labor Economics
    ).

Related distributions

  • If (
    Uniform distribution (continuous)
    ) then
  • If then
  • If and then
  • The cumulative distribution function of the Frechet distribution solves the maximum stability postulate equation
  • If then its reciprocal is Weibull-distributed:

Properties

See also

References

Further reading

External links