Fréchet distribution

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Template:Short description Template:Probability distribution

The Fréchet distribution, also known as inverse Weibull distribution,[1][2] is a special case of the generalized extreme value distribution. It has the cumulative distribution function

 Pr( Xx )=exα if x>0.

where Template:Nobr is a shape parameter. It can be generalised to include a location parameter Template:Mvar (the minimum) and a scale parameter Template:Nobr with the cumulative distribution function

 Pr( Xx )=exp[ ( xm s)α ] if x>m.

Named for Maurice Fréchet who wrote a related paper in 1927,[3] further work was done by Fisher and Tippett in 1928 and by Gumbel in 1958.[4][5]

Characteristics

The single parameter Fréchet, with parameter  α , has standardized moment

μk=0xkf(x) dx=0tkαet dt ,

(with  t=xα ) defined only for  k<α :

 μk=Γ(1kα) 

where  Γ(z)  is the Gamma function.

In particular:

  • For α>1 the expectation is E[X]=Γ(11α)
  • For α>2 the variance is Var(X)=Γ(12α)(Γ(11α))2.

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

qy=F1(y)=(logey)1α.

In particular the median is:

q1/2=(loge2)1α.

The mode of the distribution is (αα+1)1α.

Especially for the 3-parameter Fréchet, the first quartile is q1=m+slog(4)α and the third quartile q3=m+slog(43)α.

Also the quantiles for the mean and mode are:

F(mean)=exp(Γα(11α))
F(mode)=exp(α+1α).

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). Template: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.[7]
  • 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 Zi=1/logFi(Xi) and then mapping from Cartesian to pseudo-polar coordinates (R,W)=(Z1+Z2,Z1/(Z1+Z2)). Values of R1 correspond to the extreme data for which at least one component is large while W 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).


Scaling relations
  • If  XFrechet( α,s,m=0 )  then its reciprocal is Weibull-distributed:   1 XWeibull( k=α,λ=1s ) 
  • If  XFrechet(α,s,m)  then  k X+bFrechet( α,ks,k m+b ) 
  • If  XiFrechet( α,s,m )  and  Y=max{ X1,,Xn }  then  YFrechet( α,n1αs,m ) 

Properties

See also

Template:More footnotes needed

References

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Further reading

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