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dc.contributor.authorWidmann. Martines_ES
dc.contributor.authorBedia Jiménez, Joaquín es_ES
dc.contributor.authorGutiérrez Llorente, José Manueles_ES
dc.contributor.authorBosshard, Thomases_ES
dc.contributor.authorHertig, Elkees_ES
dc.contributor.authorMaraun, Douglases_ES
dc.contributor.authorCasado, María J.es_ES
dc.contributor.authorRamos, Petraes_ES
dc.contributor.authorCardoso, Rita Margaridaes_ES
dc.contributor.authorSoares, Pedro M.M.es_ES
dc.contributor.authorRibalaygua, Jaimees_ES
dc.contributor.authorPagé, Christianes_ES
dc.contributor.authorFischer, Andreas M.es_ES
dc.contributor.authorHerrera García, Sixto es_ES
dc.contributor.authorHuth, Radanes_ES
dc.contributor.otherUniversidad de Cantabriaes_ES
dc.date.accessioned2020-02-04T17:43:25Z
dc.date.available2020-02-04T17:43:25Z
dc.date.issued2019-01-31es_ES
dc.identifier.issn0899-8418es_ES
dc.identifier.issn1097-0088es_ES
dc.identifier.urihttp://hdl.handle.net/10902/18083
dc.description.abstractThe spatial dependence of meteorological variables is crucial for many impacts, for example, droughts, floods, river flows, energy demand, and crop yield. There is thus a need to understand how well it is represented in downscaling (DS) products. Within the COST Action VALUE, we have conducted a comprehensive analysis of spatial variability in the output of over 40 different DS methods in a perfect predictor setup. The DS output is evaluated against daily precipitation and temperature observations for the period 1979?2008 at 86 sites across Europe and 53 sites across Germany. We have analysed the dependency of correlations of daily temperature and precipitation series at station pairs on the distance between the stations. For the European data set, we have also investigated the complexity of the downscaled data by calculating the number of independent spatial degrees of freedom. For daily precipitation at the German network, we have additionally evaluated the dependency of the joint exceedance of the wet day threshold and of the local 90th percentile on the distance between the stations. Finally, we have investigated regional patterns of European monthly precipitation obtained from rotated principal component analysis. We analysed Perfect Prog (PP) methods, which are based on statistical relationships derived from observations, as well as Model Output Statistics (MOS) approaches, which attempt to correct simulated variables. In summary, we found that most PP DS methods, with the exception of multisite analog methods and a method that explicitly models spatial dependence yield unrealistic spatial characteristics. Regional climate model?based MOS methods showed good performance with respect to correlation lengths and the joint occurrence of wet days, but a substantial overestimation of the joint occurrence of heavy precipitation events. These findings apply to the spatial scales that are resolved by our observation network, and similar studies with higher resolutions, which are relevant for small hydrological catchment, are desirable.es_ES
dc.description.sponsorshipFunding Information: EU. Grant Number: EU COST Action ES1102es_ES
dc.format.extent27 p.es_ES
dc.language.isoenges_ES
dc.publisherJohn Wiley and Sons Ltdes_ES
dc.rights©John Wiley & Sons. ""This is the peer reviewed version of the following article: [FULL CITE], which has been published in final form at https://rmets.onlinelibrary.wiley.com/doi/epdf/10.1002/joc.6024. This article may be used for non-commercial purposes in accordance with Wiley Terms and Conditions for Self-Archiving."es_ES
dc.sourceInternational Journal of Climatology Volume 39, Issue 9 July 2019 Pages 3819-3845es_ES
dc.titleValidation of spatial variability in downscaling results from the VALUE perfect predictor experimentes_ES
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.relation.publisherVersionhttps://rmets.onlinelibrary.wiley.com/doi/epdf/10.1002/joc.6024es_ES
dc.rights.accessRightsopenAccesses_ES
dc.identifier.DOI10.1002/joc.6024es_ES
dc.type.versionacceptedVersiones_ES


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