2016
DOI: 10.1515/acgeo-2015-0070
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Comparison of Two Nonstationary Flood Frequency Analysis Methods within the Context of the Variable Regime in the Representative Polish Rivers

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Cited by 22 publications
(22 citation statements)
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References 32 publications
(26 reference statements)
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“…It can be done by assuming trends in explicit distribution parameters or in distribution moments, more precisely in the mean and the standard deviation. The second method is recommended (Strupczewski and Kaczmarek 2001;Kochanek et al 2013;Strupczewski et al 2016). It enables mutual comparisons of the results obtained by different models and the classical climatological approach based on analysis of the variation of the mean and the standard deviation of climatic data over time.…”
Section: Methodology Seasonal Approachmentioning
confidence: 99%
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“…It can be done by assuming trends in explicit distribution parameters or in distribution moments, more precisely in the mean and the standard deviation. The second method is recommended (Strupczewski and Kaczmarek 2001;Kochanek et al 2013;Strupczewski et al 2016). It enables mutual comparisons of the results obtained by different models and the classical climatological approach based on analysis of the variation of the mean and the standard deviation of climatic data over time.…”
Section: Methodology Seasonal Approachmentioning
confidence: 99%
“…The method used for the assessment of the seasonal time dependent upper quantile is an adaptation of the so called two-stage (TS) method presented by, e.g., Strupczewski et al (2016). The TS method consists of two stages:…”
Section: Two-stage Methodsmentioning
confidence: 99%
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“…The RB and the RRMSE were calculated for 10,000 simulations with a sample size of n = 50, 100 and 200 generated by considered parent distribution. Compared to the weighted least squares (WLS), described in Strupczewski and Kaczmarek (2001), Kochanek et al (2013) and Strupczewski et al (2015), the algorithm GAMLSS showed better efficiency in the estimation of the trend in the standard deviation and worse in the mean value. This finding also applies to the real flood data when sometimes the algorithm GAMLSS identified the trend in the mean as the opposite to that observed.…”
Section: Hydrological Applications and Assessment Of The Gamlss Softwarementioning
confidence: 99%