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The underestimation of probability of extreme rainfall and flood by prevailing statistical methodologies and how to avoid it

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dc.contributor.author Koutsoyiannis, D en
dc.date.accessioned 2014-03-01T02:54:13Z
dc.date.available 2014-03-01T02:54:13Z
dc.date.issued 2006 en
dc.identifier.uri https://dspace.lib.ntua.gr/xmlui/handle/123456789/36720
dc.title The underestimation of probability of extreme rainfall and flood by prevailing statistical methodologies and how to avoid it en
heal.type conferenceItem en
heal.publicationDate 2006 en
heal.abstract Probabilistic modelling of extreme rainfall has a crucial role in flood risk estimation and consequently in the design and management of flood protection works. This is particularly the case for urban floods, where the plethora of flow control sites and the scarcity of flow measurements make the use of rainfall data indispensable. For half a century, the Gumbel distribution has been the prevailing model of extreme rainfall. Several arguments including theoretical reasons and empirical evidence are supposed to support the appropriateness of the Gumbel distribution, which corresponds to an exponential parent distribution tail. Recently, the applicability of this distribution has been criticized both on theoretical and empirical grounds. Thus, new theoretical arguments based on comparisons of actual and asymptotic extreme value distributions as well as on the principle of maximum entropy indicate that the Extreme Value Type 2 distribution should replace the Gumbel distribution. In addition, several empirical analyses using long rainfall records (e.g. a recent study of annual maximum daily rainfall from 169 stations from Europe and the USA, with lengths exceeding 100 years) agree with the new theoretical findings. Furthermore, the empirical analyses show that the Gumbel distribution may significantly underestimate the largest extreme rainfall amounts (albeit its predictions for small return periods of 5-10 years are satisfactory), whereas this distribution would seem as an appropriate model if fewer years of measurements were available (i.e., parts of the long records were used). en


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