Geoscience Reference
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a
b
Fig. 3.10 a Probability density function f ( x ), and b cumulative distribution function F ( x ), of a
Fisher's F distribution with dif erent values for ʦ1 and ʦ2.
of freedom. In the analysis of univariate data this distribution has n -1
degrees of freedom, where n is the sample size. As ʦ→∞, the t distribution
converges towards the standard normal distribution. Since the t distribution
approaches the normal distribution for ʦ>30, it is rarely used for distribution
i tting. However, the t distribution is used for hypothesis testing using the
t -test (Section 3.7).
Fisher's F Distribution
h e F distribution was named at er the statistician Sir Ronald Fisher (1890-
1962). It is used for hypothesis testing using the F -test (Section 3.8). h e F
distribution has a relatively complex probability density function (Fig. 3.10):
where x >0 and ʓ is again the Gamma function. h e two parameters ʦ 1 and
ʦ 2 are the numbers of degrees of freedom.
χ 2 or Chi-Squared Distribution
h e ˇ 2 distribution was introduced by Friedrich Helmert (1876) and Karl
Pearson (1900). It is not used for i tting a distribution but has important
applications in statistical hypothesis testing using the ˇ 2 -test (Section 3.9).
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