P.: The statistical distribution of meteorological outliers, Geophys

[1] A general expression for the statistical distribution of the probability of the highest event occurring in a record is presented. This result can be empirically applied to situations where records are available for multiple geographical locations. The empirical estimation of the probability of t...

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Main Authors: H. W. Van Den Brink, G. P. Können
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
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Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.549.2297
http://www.knmi.nl/publications/fulltexts/2008gl035967.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.549.2297 2023-05-15T17:32:19+02:00 P.: The statistical distribution of meteorological outliers, Geophys H. W. Van Den Brink G. P. Können The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.549.2297 http://www.knmi.nl/publications/fulltexts/2008gl035967.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.549.2297 http://www.knmi.nl/publications/fulltexts/2008gl035967.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.knmi.nl/publications/fulltexts/2008gl035967.pdf text ftciteseerx 2016-01-08T11:26:03Z [1] A general expression for the statistical distribution of the probability of the highest event occurring in a record is presented. This result can be empirically applied to situations where records are available for multiple geographical locations. The empirical estimation of the probability of the highest events provides a means to assess whether the assumed (extreme value) distribution is appropriate for extrapolation or not. The approach allows for combining the highest events from different records and to validate estimated return periods in the order of the length of the combined records. The method is illustrated with an analysis of the annual extreme wind speeds over the North Atlantic area according to the ERA40 dataset, showing that the Gumbel distribution is in favor of the GEV distribution to estimate the (appropriately transformed) extreme wind speeds up to return periods of 104 years. Citation: van den Text North Atlantic Unknown
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description [1] A general expression for the statistical distribution of the probability of the highest event occurring in a record is presented. This result can be empirically applied to situations where records are available for multiple geographical locations. The empirical estimation of the probability of the highest events provides a means to assess whether the assumed (extreme value) distribution is appropriate for extrapolation or not. The approach allows for combining the highest events from different records and to validate estimated return periods in the order of the length of the combined records. The method is illustrated with an analysis of the annual extreme wind speeds over the North Atlantic area according to the ERA40 dataset, showing that the Gumbel distribution is in favor of the GEV distribution to estimate the (appropriately transformed) extreme wind speeds up to return periods of 104 years. Citation: van den
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author H. W. Van Den Brink
G. P. Können
spellingShingle H. W. Van Den Brink
G. P. Können
P.: The statistical distribution of meteorological outliers, Geophys
author_facet H. W. Van Den Brink
G. P. Können
author_sort H. W. Van Den Brink
title P.: The statistical distribution of meteorological outliers, Geophys
title_short P.: The statistical distribution of meteorological outliers, Geophys
title_full P.: The statistical distribution of meteorological outliers, Geophys
title_fullStr P.: The statistical distribution of meteorological outliers, Geophys
title_full_unstemmed P.: The statistical distribution of meteorological outliers, Geophys
title_sort p.: the statistical distribution of meteorological outliers, geophys
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.549.2297
http://www.knmi.nl/publications/fulltexts/2008gl035967.pdf
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http://www.knmi.nl/publications/fulltexts/2008gl035967.pdf
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