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dc.contributor.authorSneyers, R.
dc.coverage.temporal20th century
dc.date1961
dc.date.accessioned2016-03-07T17:14:04Z
dc.date.accessioned2021-12-09T09:52:40Z
dc.date.available2016-03-07T17:14:04Z
dc.date.available2021-12-09T09:52:40Z
dc.identifier.urihttps://orfeo.belnet.be/handle/internal/8382
dc.descriptionThe classical extreme-value theory does not give a good account of the distribution of maximum rainfall intensities in Belgium. Reasons are given for the use, in this case, of a probability function defined by a double exponential whose argument is a function represented by a curve with two asymptotes. The application of such a probability function, when the curve is a branch of a hyperbola, to the maximum rainfall, in 1 min.; at Uccle, leads to a good fit.
dc.languageeng
dc.publisherIRM
dc.publisherKMI
dc.publisherRMI
dc.relation.ispartofseriesContributions, n° - Bijdragen, nr.
dc.titleOn a special distribution of maximum values
dc.typeBook
dc.subject.frascatiEarth and related Environmental sciences
dc.audienceGeneral Public
dc.audienceScientific
dc.subject.freeRainfall
dc.subject.freeBelgium
dc.subject.freeHyperbola
dc.subject.freeUccle
dc.source.volume65
dc.source.page4
Orfeo.peerreviewedYes


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