2003
DOI: 10.1623/hysj.48.6.917.51427
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Divergence criteria in extreme rainfall series frequency analyses

Abstract: Extreme rainfall series (ERS) are treated as successive-duration events of from 5 min to 24 h in most parts of the world. In Turkey, as in European countries, the ERS of standard durations of 5, 10, 15, 30, 60 min, and 2, 3, 4, 5, 6, 8, 12, 18, 24 h are recorded, and these sample series are analysed to ultimately determine the depthduration-frequency (DDF) relationships. If a probability distribution function (pdf) is used for these ERS, the frequency curves in the form of graphical quantile functions may int… Show more

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Cited by 7 publications
(8 citation statements)
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“…One other plausible reason for the possible crossover of IDF curves is that frequency analysis of rainfall data is performed separately for each duration without considering the inter-correlations that are intrinsically embedded in rainfall data of different durations. Haktanir [53] earlier pointed out that rainfall frequency analysis of different durations in the process of establishing IDF relationships should not be performed independently of each other, but did not propose a mechanism to handle the correlation directly. Recently, Gräler et al [54] applied D-vine copula, along with the generalized extreme value distributions, to derive rainfall IDF relationships based on rainfalls of five durations.…”
Section: Numerical Examplementioning
confidence: 99%
“…One other plausible reason for the possible crossover of IDF curves is that frequency analysis of rainfall data is performed separately for each duration without considering the inter-correlations that are intrinsically embedded in rainfall data of different durations. Haktanir [53] earlier pointed out that rainfall frequency analysis of different durations in the process of establishing IDF relationships should not be performed independently of each other, but did not propose a mechanism to handle the correlation directly. Recently, Gräler et al [54] applied D-vine copula, along with the generalized extreme value distributions, to derive rainfall IDF relationships based on rainfalls of five durations.…”
Section: Numerical Examplementioning
confidence: 99%
“…But, the frequency analyses of the 14 successive‐duration annual extreme rainfalls series should not be performed independently from each other. The magnitude of extreme rainfall, x 2 , of a longer‐duration, tr 2 , should be greater than that of extreme rainfall, x 1 , of shorter‐duration, tr 1 , both having the same average return period, T , which necessitate that the quantile function of the tr 2 ‐duration annual extreme rainfall must be divergent from that of the tr 1 ‐duration annual extreme rainfall with increasing return periods, as analytically depicted by the following constraints (Haktanir, 2003b): …”
Section: Divergence Criterionmentioning
confidence: 99%
“…Inequality (1) is the revelation of conservation of mass, and inequality (2) assures the frequency curves of successive‐duration annual extreme rainfall series to be diverging from each other with increasing return periods up to T of + ∞ years. Inequalities (1) and (2) define the divergence criterion, and accordingly, the magnitudes of the parameters of the adopted probability distribution for the 14 successive‐duration annual extreme rainfalls must be either increasing or decreasing with increasing rainfall duration, tr (Haktanir, 2003b).…”
Section: Divergence Criterionmentioning
confidence: 99%
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“…The generalization approach proposed herein provides the following advantages and innovations for the IDF relationships: In order for the IDF curves not to exhibit 'intersections' in a guaranteed way, both sample mean and sample standard deviation must show increasing trends with increasing rainfall duration. This is called 'divergence criterion' (Haktanir 2003). This criterion is defined as the constraints to be fulfilled by the parameters of a parent distribution in order not to intersect each others with increasing return periods.…”
Section: Introductionmentioning
confidence: 99%