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dc.contributor.authorMatteo, Aurora
dc.contributor.authorGarnés Morales, Ginés
dc.contributor.authorMoreno, Alberto
dc.contributor.authorRibeiro, Andreia
dc.contributor.authorAzorín Molina, César
dc.contributor.authorBedía Jiménez, Joaquín
dc.contributor.authorDi Giuseppe, Francesca
dc.contributor.authorDunn, Robert J.H.
dc.contributor.authorHerrera García, Sixto 
dc.contributor.authorProvenzale, Antonello
dc.contributor.authorQuilcaille, Yann
dc.contributor.authorTorres Vázquez, Miguel Ángel
dc.contributor.authorTurco, Marco
dc.contributor.otherUniversidad de Cantabriaes_ES
dc.date.accessioned2025-09-12T14:42:02Z
dc.date.available2025-09-12T14:42:02Z
dc.date.issued2025-07-28
dc.identifier.issn2397-3722
dc.identifier.otherPID2021-123193OB-I00es_ES
dc.identifier.otherPID2023-149997OA-I00es_ES
dc.identifier.urihttps://hdl.handle.net/10902/37166
dc.description.abstractThe Canadian Fire Weather Index (FWI), widely used to assess wildfire danger, typically relies on noonspecific meteorological data. However, climate models often provide only daily aggregated values, posing a challenge for accurate FWI calculations.Weevaluated daily approximations for FWI95d-the annual count of extreme fire-weather days-against the standard noon-based method (1980-2023). Our findings reveal that noon-based FWI95d show a global increase of ~65% (11.66 days over 44 years). In contrast, daily approximations tend to overestimate these trends by 5-10%, with combinations involving minimum relative humidity showing the largest divergences. Globally, up to 15 million km²-particularly in the western United States, southern Africa, and parts of Asia-exhibit significant overestimations. We recommend (i) prioritizing the inclusion of sub-daily meteorological data in future climatemodel intercomparison projects to enhanceFWI accuracy, and (ii) adopting daily mean approximations as the least-biased alternative if noon-specific data are unavailable.es_ES
dc.description.sponsorshipThe authors wish to acknowledge the anonymous reviewers for their detailed and helpful comments to the original manuscript. This work was supported by the project ‘Climate and Wildfire Interface Study for Europe (CHASE)’ under the 6th Seed Funding Call by the European University for Well-Being (EUniWell). M.T. acknowledges funding by the Spanish Ministry of Science, Innovation and Universities through the Ramón y Cajal Grant Reference RYC2019-027115-I and through the project ONFIRE, Grant PID2021-123193OB-I00, funded by MCIN/AEI/10.13039/501100011033 and by “ERDF A way of making Europe”. A.P. acknowledges the support of the EU H2020 project “FirEUrisk”, Grant Agreement No. 101003890. Y.Q. acknowledges the support of the EU Horizon Europe project SPARCCLE, Grant Agreement No. 101081369. RJHD was supported by the Met Office Hadley Centre Climate Programme funded by DSIT. C.A-M. received funding from the PROMETEO Ref. CIPROM/2023/38. A.F.S.R. acknowledges the Alexander von Humboldt Foundation (AvH) for a postdoctoral fellowship and the Deutsche Forschungsgemeinschaft (DFG) - Project number 530175554. J.B. has received research support from Grant PID2023-149997OA-I00 (PROTECT Project) funded by MICIU/AEI/10.13039/501100011033 and by ERDF/EU.es_ES
dc.format.extent8 p.es_ES
dc.language.isoenges_ES
dc.publisherSpringer Naturees_ES
dc.rights© The Author(s) 2025. Open Access This article is licensed under a Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International Licensees_ES
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/4.0/*
dc.sourcenpj Climate and Atmospheric Science, 2025, 8, 284es_ES
dc.titleChallenges in assessing Fire Weather changes in a warming climatees_ES
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.relation.publisherVersionhttps://doi.org/10.1038/s41612-025-01163-0es_ES
dc.rights.accessRightsopenAccesses_ES
dc.relation.projectIDinfo:eu-repo/grantAgreement/AEI/Plan Estatal de Investigación Científica y Técnica y de Innovación 2021-2023/PID2021-123193OB-I00/ES/ON THE CLIMATE-DRIVEN EVOLUTION OF FIRES ACROSS TIME SCALES AND REGIONS WORLDWIDE/es_ES
dc.relation.projectIDinfo:eu-repo/grantAgreement/AEI/Plan Estatal de Investigación Científica y Técnica y de Innovación 2021-2023/PID2023-149997OA-I00/ES/PROYECCIONES DEL CAMBIO CLIMATICO DE CONFORT HUMANO MEDIANTE TECNICAS DE REGIONALIZACION DINAMICA Y EMULADORES BASADOS EN APRENDIZAJE PROFUNDO/es_ES
dc.identifier.DOI10.1038/s41612-025-01163-0
dc.type.versionpublishedVersiones_ES


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