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dc.contributor.authorRodríguez Solá, Raúl
dc.contributor.authorCasas Castillo, M. del Carmen
dc.contributor.authorNavarro Bosque, Javier
dc.contributor.authorRedaño Xipell, Angel
dc.contributor.otherUniversitat Politècnica de Catalunya. Departament de Física
dc.coverage.spatialeast=2.124180793762207; north=41.41841731420638; name=Observatori Fabra, 27, 08035 Barcelona, Espanya
dc.coverage.spatialeast=0.4951894283294678; north=40.82083264664586; name=Observatori de l'Ebre, Tarragona, Espanya
dc.coverage.spatialeast=-3.686063289642334; north=40.40727115029358; name=Obserbatorio del Retiro, Madrid, Espanya
dc.date.accessioned2016-05-25T10:38:08Z
dc.date.available2017-04-20T00:30:34Z
dc.date.issued2016-04-20
dc.identifier.citationRodriguez, R., M. Carmen Casas-Castillo, Navarro, J., Redaño, A. A study of the scaling properties of rainfall in spain and its appropriateness to generate intensity-duration-frequency curves from daily records. "International journal of climatology", 20 Abril 2016.
dc.identifier.issn0899-8418
dc.identifier.urihttp://hdl.handle.net/2117/87312
dc.description.abstractA methodology based on the fractal properties of rainfall has been applied to obtain the intensity-duration-frequency, IDF, curves for 100 pluviometric Spanish stations over the Iberian Peninsula and the Balearic Islands from their daily precipitation series. The scaling behaviour of maximum rainfall intensities has been investigated and simple scaling has resulted suitable. This methodology has been verified in three emblematic observatories with available sub-daily registers and current known generalized IDF relationships: the Fabra Observatory of Barcelona, the Ebre Observatory near Tortosa (Tarragona) and the Retiro Observatory of Madrid. Despite some general concordance with the mean annual rainfall distribution over Spain, the spatial distribution of the scaling parameter found for the 100 stations shows some discrepancies in diverse areas probably due to the influence of other features, as the inter-annual rainfall variability and the contribution of convective rainfall to total precipitation, on the characteristic rainfall pattern in these areas.
dc.language.isoeng
dc.publisherJohn Wiley & Sons
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/
dc.subjectÀrees temàtiques de la UPC::Física
dc.subject.lcshRain and rainfall
dc.subject.lcshRainfall frequencies
dc.subject.lcshFractals
dc.subject.otherSimple scaling
dc.subject.otherFractal analysis
dc.subject.otherRainfall intensity
dc.subject.otherIntensity-duration-frequency curves
dc.titleA study of the scaling properties of rainfall in spain and its appropriateness to generate intensity-duration-frequency curves from daily records
dc.typeArticle
dc.subject.lemacPluviometria (Meteorologia)
dc.subject.lemacFractals
dc.identifier.doi10.1002/joc.4738
dc.relation.publisherversionhttp://onlinelibrary.wiley.com/doi/10.1002/joc.4738/full
dc.rights.accessOpen Access
local.identifier.drac17722506
dc.description.versionPostprint (author's final draft)
local.citation.authorRodriguez, R.; Casas-Castillo, M. Carmen; Navarro, J.; Redaño, A.
local.citation.publicationNameInternational journal of climatology


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