2016
DOI: 10.3176/earth.2016.15
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Modelling precipitation extremes in the Czech Republic: update of intensity–duration–frequency curves

Abstract: Precipitation records from six stations of the Czech Hydrometeorological Institute were subject to statistical analysis with the objectives of updating the intensity-duration-frequency (IDF) curves, by applying extreme value distributions, and comparing the updated curves against those produced by an empirical procedure in 1958. Another objective was to investigate differences between both sets of curves, which could be explained by such factors as different measuring instruments, measuring stations altitudes … Show more

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Cited by 2 publications
(5 citation statements)
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“…As mentioned above, the Gumbel distribution most likely underestimates the largest extremes. Additionally, the increase in extreme hydrological events strengthens the importance of updating the methodology, as also shown for other locations (e.g., [26,27]). We therefore propose to abandon the Gumbel distribution, and introduce two methods of fitting the GEV distribution to annual maxima: a modified Maximum Likelihood (ML) estimation [28] and Bayesian inference (e.g., [16,29,30]).…”
Section: Introductionsupporting
confidence: 62%
“…As mentioned above, the Gumbel distribution most likely underestimates the largest extremes. Additionally, the increase in extreme hydrological events strengthens the importance of updating the methodology, as also shown for other locations (e.g., [26,27]). We therefore propose to abandon the Gumbel distribution, and introduce two methods of fitting the GEV distribution to annual maxima: a modified Maximum Likelihood (ML) estimation [28] and Bayesian inference (e.g., [16,29,30]).…”
Section: Introductionsupporting
confidence: 62%
“…In case of very short time series it is also possible to estimate the maximum N-year precipitation, but using different methods (the POT method supplemented by the bootstrapping methods), as shown in , Fusek et al (2016) etc.…”
Section: Generalized Extreme Value Distribution (Gev)mentioning
confidence: 99%
“…1) Creation of annual maximum series (AMS) for all the stations 2) Determination of N-year design precipitation for all the stations by two methods: by the GEV distribution and the Gumbel distribution. Specialized software was used in the calculations -ProClimDB (Štěpánek, 2010) and EVDest 1.0 (Fusek and Holešovský, 2014). EVDest software contains only estimates of GEV distribution, which is preferred in modern hydrology.…”
Section: Analytical Proceduresmentioning
confidence: 99%
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