On accuracy of upper quantiles estimation

Flood frequency analysis (FFA) entails the estimation of the upper tail of a probability density function (PDF) of annual peak flows obtained from either the annual maximum series or partial duration series. In hydrological practice, the properties of various methods of upper quantiles estimation ar...

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Main Authors: I. Markiewicz, W. G. Strupczewski, K. Kochanek
Format: Article
Language:English
Published: Copernicus Publications 2010-11-01
Series:Hydrology and Earth System Sciences
Online Access:http://www.hydrol-earth-syst-sci.net/14/2167/2010/hess-14-2167-2010.pdf
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spelling doaj-a2b5f4dc2f5e4c8d96b9eb4c8046e4152020-11-24T22:22:39ZengCopernicus PublicationsHydrology and Earth System Sciences1027-56061607-79382010-11-0114112167217510.5194/hess-14-2167-2010On accuracy of upper quantiles estimationI. MarkiewiczW. G. StrupczewskiK. KochanekFlood frequency analysis (FFA) entails the estimation of the upper tail of a probability density function (PDF) of annual peak flows obtained from either the annual maximum series or partial duration series. In hydrological practice, the properties of various methods of upper quantiles estimation are identified with the case of known population distribution function. In reality, the assumed hypothetical model differs from the true one and one cannot assess the magnitude of error caused by model misspecification in respect to any estimated statistics. The opinion about the accuracy of the methods of upper quantiles estimation formed from the case of known population distribution function is upheld. The above-mentioned issue is the subject of the paper. The accuracy of large quantile assessments obtained from the four estimation methods is compared to two-parameter log-normal and log-Gumbel distributions and their three-parameter counterparts, i.e., three-parameter log-normal and GEV distributions. The cases of true and false hypothetical models are considered. The accuracy of flood quantile estimates depends on the sample size, the distribution type (both true and hypothetical), and strongly depends on the estimation method. In particular, the maximum likelihood method loses its advantageous properties in case of model misspecification. http://www.hydrol-earth-syst-sci.net/14/2167/2010/hess-14-2167-2010.pdf
collection DOAJ
language English
format Article
sources DOAJ
author I. Markiewicz
W. G. Strupczewski
K. Kochanek
spellingShingle I. Markiewicz
W. G. Strupczewski
K. Kochanek
On accuracy of upper quantiles estimation
Hydrology and Earth System Sciences
author_facet I. Markiewicz
W. G. Strupczewski
K. Kochanek
author_sort I. Markiewicz
title On accuracy of upper quantiles estimation
title_short On accuracy of upper quantiles estimation
title_full On accuracy of upper quantiles estimation
title_fullStr On accuracy of upper quantiles estimation
title_full_unstemmed On accuracy of upper quantiles estimation
title_sort on accuracy of upper quantiles estimation
publisher Copernicus Publications
series Hydrology and Earth System Sciences
issn 1027-5606
1607-7938
publishDate 2010-11-01
description Flood frequency analysis (FFA) entails the estimation of the upper tail of a probability density function (PDF) of annual peak flows obtained from either the annual maximum series or partial duration series. In hydrological practice, the properties of various methods of upper quantiles estimation are identified with the case of known population distribution function. In reality, the assumed hypothetical model differs from the true one and one cannot assess the magnitude of error caused by model misspecification in respect to any estimated statistics. The opinion about the accuracy of the methods of upper quantiles estimation formed from the case of known population distribution function is upheld. The above-mentioned issue is the subject of the paper. The accuracy of large quantile assessments obtained from the four estimation methods is compared to two-parameter log-normal and log-Gumbel distributions and their three-parameter counterparts, i.e., three-parameter log-normal and GEV distributions. The cases of true and false hypothetical models are considered. The accuracy of flood quantile estimates depends on the sample size, the distribution type (both true and hypothetical), and strongly depends on the estimation method. In particular, the maximum likelihood method loses its advantageous properties in case of model misspecification.
url http://www.hydrol-earth-syst-sci.net/14/2167/2010/hess-14-2167-2010.pdf
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