2014
DOI: 10.1061/(asce)he.1943-5584.0000942
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Comparison between Parametric and Nonparametric Approaches for the Calculation of Two Drought Indices: SPI and SSI

Abstract: can directly trigger a drought, unlike other natural hazards, with exacerbating factors such as overfarming, excessive irrigation, deforestation, and overexploiting available water (Wilhite 2000). In order to monitor the dynamics of droughts, several indices have been developed, accommodating the different typologies of droughts.

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Cited by 56 publications
(26 citation statements)
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“…This methodological issue is addressed in this paper by assigning SPI values for zero precipitation based on the ‘centre of mass’ of the zero distribution rather than the maximum probability, thereby producing SPI values that maintain statistical interpretability (mean, μ = 0). The concept of ‘probability mass’ when normalizing zeros in the SPI was discussed in Solakova et al (), although the implementation in this paper eventually used the former method discussed above. In the ‘proposed’ method for normalizing zero precipitation, the likelihood of zero precipitation is calculated based on the empirical cumulative distribution.…”
Section: Methodsmentioning
confidence: 99%
“…This methodological issue is addressed in this paper by assigning SPI values for zero precipitation based on the ‘centre of mass’ of the zero distribution rather than the maximum probability, thereby producing SPI values that maintain statistical interpretability (mean, μ = 0). The concept of ‘probability mass’ when normalizing zeros in the SPI was discussed in Solakova et al (), although the implementation in this paper eventually used the former method discussed above. In the ‘proposed’ method for normalizing zero precipitation, the likelihood of zero precipitation is calculated based on the empirical cumulative distribution.…”
Section: Methodsmentioning
confidence: 99%
“…This issue can be addressed by using the Weibull plotting position function (Equation (1)) to estimate the probability of zero precipitation. Further information about this latter method, which is based on the concept of 'centre of mass' and was applied in this study, can be found in Solakova et al (2014).…”
Section: Cumulative Distribution Functions and Zero Precipitation Valuesmentioning
confidence: 99%
“…Sometimes it is hard to discriminate among canonical forms of FXw(x), or they may not provide a good fit to the data (Soláková et al 2014;Lall et al, 2016). On the other hand, using different distribution functions could lead to different tail behavior and thus inconsistencies in characteristics of extremes across space .…”
Section: Spi and Ssi Indicesmentioning
confidence: 99%