Gumbel Distribution for Extreme Values ◾ 327
Type III (Weibull)
G x e x b
G x x b
x b
a
( )
( )
= <
= ≥
− −
−
− α
1
(20.6)
Although the behavior of the three laws is completely different, they can
be combined into a single parameterization containing one parameter ξ that
controls the “heaviness” of the tail, called the shape parameter:
GEV G x e
x
( ) =
− +
−
−
1
1
ξ
µ
σ
ξ
(20.7)
e location parameter μ determines where the distribution is concen-
trated. e scale parameter σ determines its width. e shape parameter ξ
determines the rate of tail decay (the larger ξ, the heavier the tail), with the
following:
ξ > 0 indicating the heavy-tailed (Fréchet) case.
ξ = 0 indicating the light-tailed (Gumbel) case.
ξ < 0 indicating the truncated distribution (Weibull) case.
e extreme value distributions have been differently adopted by different
users. Each type of distribution offers certain advantages over the others for
specific cases.
In earthquake modeling, Zimbidis et al. [4] preferred to use type III
extreme value distribution (Weibull). ey analyzed the annual maximum
magnitude of earthquakes in Greece during the period 1966–2005. e plot
of mean excess over a threshold indicates a very short tail, and researchers
have chosen Weibull accordingly.
In worst-case execution time analysis of real-time embedded systems, Lu
et al. [5] used the Gumbel distribution after selecting the data very care-
fully using special sampling techniques. eir predictions agree closely with
observed data.
However, in the probabilistic minimum interarrival time analysis of
embedded systems, Maxim et al. [6] found that the Weibull extreme value
distribution fits better.
During the analysis of wave data, Caires [7] found the general extreme
value model more suitable.
e choice depends on data.