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dc.contributor.authorHerrera García, Sixto 
dc.contributor.authorSoares, P. M. M.
dc.contributor.authorCardoso, Rita Margarida
dc.contributor.authorGutiérrez Llorente, José Manuel
dc.contributor.otherUniversidad de Cantabriaes_ES
dc.date.accessioned2020-11-26T08:21:00Z
dc.date.available2020-12-31T03:45:10Z
dc.date.issued2020-06
dc.identifier.issn2169-897X
dc.identifier.issn2169-8996
dc.identifier.issn2156-2202
dc.identifier.otherCGL2010-21869es_ES
dc.identifier.otherCGL2010-22158-C02es_ES
dc.identifier.urihttp://hdl.handle.net/10902/19907
dc.description.abstractABSTRACT: This work evaluates the daily precipitation and mean temperature of eight CORDEX-EUR11 ERA-Interim-driven simulations of EURO-CORDEX over the Iberian Peninsula (IP) for the period 1989-2008. To this aim, three observational data sets (Iberia01, E-OBS-v19e, and MESAN-0.11) were considered as reference and compared with the models by means of several indices reflecting the mean and extreme regimes over the IP. For precipitation the Lamb weather types were considered to identify synoptic conditions related with higher observational uncertainty. RCMs are able to reproduce the spatial pattern and the variability observed in the IP. However, there is a higher agreement between models and observations for mean temperature than for precipitation, decreasing when extremes are analyzed. For the observational uncertainty analysis, also extreme daily temperatures were considered to obtain a wider picture of this topic. A higher dependence on the observational data set has been found for precipitation than for temperature. This uncertainty is particularly significant when the 50-year return value is considered for which the observational uncertainty doubles the model uncertainty. Only the wet-day frequency presents values lower than 0.5 for all seasons, with most of the rest of values reflecting a similar contribution of both components to the uncertainty. In the case of temperatures, the main contribution of the observations has been found when the lower (MAE01) and upper (MAE99) extremes are considered, with values lower than 0.5. For precipitation the observational uncertainty increases when synoptic patterns affecting the Mediterranean Basin are considered, reflecting the difficulty to properly capture the Mediterranean precipitation regimes.es_ES
dc.description.sponsorshipThis work was partially funded by the Spanish Government R&D Programme (Exp. CGL2010-21869 and CGL2010-22158-C02) and the European Comission (INDECIS: H2020-690462). Pedro M. M. Soares and Rita M. Cardoso wish to acknowledge the SOLAR (PTDC/GEOMET/7078/2014) Project and the funding by the Instituto Dom Luiz (Project FCT UID/GEO/50019/2019).es_ES
dc.format.extent16 p.es_ES
dc.language.isoenges_ES
dc.publisherJohn Wiley & Sonses_ES
dc.rights© American Geophysical Uniones_ES
dc.sourceJournal of Geophysical Research. Atmospheres Volume125, Issue12 27 June 2020 e2020JD032880es_ES
dc.titleEvaluation of the EURO-CORDEX Regional Climate Models Over the Iberian Peninsula: Observational Uncertainty Analysises_ES
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.relation.publisherVersionhttps://agupubs.onlinelibrary.wiley.com/doi/abs/10.1029/2020JD032880es_ES
dc.rights.accessRightsopenAccesses_ES
dc.relation.projectIDinfo:eu-repo/grantAgreement/EC/H2020/690462/EU/European Research Area for Climate Services/ERA4CS/es_ES
dc.identifier.DOI10.1029/2020JD032880
dc.type.versionpublishedVersiones_ES


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