2010
DOI: 10.1016/j.jspi.2009.03.026
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Asymptotics of the sample coefficient of variation and the sample dispersion

Abstract: MSC:primary 62G20 secondary 60F05 Keywords:Weak limit theorems Functions of regular variation Domain of attraction of a stable law Sample coefficient of variation Sample dispersion Student's t-statistic Extreme value theory The coefficient of variation and the dispersion are two examples of widely used measures of variation. We show that their applicability in practice heavily depends on the existence of sufficiently many moments of the underlying distribution. In particular, we offer a set of results that ill… Show more

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Cited by 33 publications
(20 citation statements)
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“…This approach is also used in de la Peña and Yang (1999). More closely related to our work, in the context of self-normalized processes, are Giné et al (1997), Fuchs and Joffe (1997), Albrecher and Teugels (2006), and Albrecher et al (2010). Proposition 1 is perhaps novel in pointing out the potential use of tilted distributions.…”
Section: A Useful Identitysupporting
confidence: 52%
“…This approach is also used in de la Peña and Yang (1999). More closely related to our work, in the context of self-normalized processes, are Giné et al (1997), Fuchs and Joffe (1997), Albrecher and Teugels (2006), and Albrecher et al (2010). Proposition 1 is perhaps novel in pointing out the potential use of tilted distributions.…”
Section: A Useful Identitysupporting
confidence: 52%
“…SF2 represents the maximum annual flow throughout the sub-period; SF3 is the minimum annual flow over the sub-period; SF4 signifies the maximum monthly flow over a single year; SF5 corresponds to the minimum monthly flow over a single year; SD and CV are statistical measures of dispersion in a data series around its mean; and the CV of annual streamflow data series represents the ratio of standard deviation to the mean annual flow. The CV is valuable in matching the degree of dispersion and variation among data series (Albrecher et al 2010;Boik and Shirvani 2009). PR corresponds to the ratio between maximum and minimum streamflow values, and it provides initial indication of seasonal variability.…”
Section: Determining the Hydrological Variablesmentioning
confidence: 99%
“…Moreover, T n is closely connected to the study of the sample coefficient of variation and the sample dispersion (cf. Albrecher, Ladoucette and Teugels [2]). …”
Section: Introductionmentioning
confidence: 98%