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Fig. 5 | Geoenvironmental Disasters

Fig. 5

From: How sample size can effect landslide size distribution

Fig. 5

The regions of acceptance for the null hypothesis that “the observed differences in power exponent (γ) between two different subsets of the same dataset is derived from random processes” at a significance level of 0.05 are shown. a, b, c, d, e and f present the results for subdividing ratio 1:1, 2:1, 3:1, 4:1, 5:1 and 6:1, respectively. Please note that some of the regions of acceptance for sample sizes less than 250 go beyond the range of this figure, because small sample size together with large subdividing ratio will yield unrealistic wide regions of acceptance

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