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dc.contributor.authorValenzuela, Pablo
dc.contributor.authorDomínguez Cuesta, María José
dc.contributor.authorPereira, Susana
dc.contributor.authorRemondo Tejerina, Juan 
dc.contributor.authorBornaetxea Estela, Txomin
dc.contributor.authorVaz, Teresa
dc.contributor.authorRivas Mantecón, María Victoria 
dc.contributor.authorBonachea Pico, Jaime 
dc.contributor.authorGonzález Díez, Alberto 
dc.contributor.authorSan Millán, Eliezer
dc.contributor.authorBateira, Carlos
dc.contributor.authorZêzere, José Luís
dc.contributor.otherUniversidad de Cantabriaes_ES
dc.date.accessioned2025-05-06T07:35:08Z
dc.date.issued2025-07
dc.identifier.issn1872-6887
dc.identifier.otherPID2021- 122472NB-100es_ES
dc.identifier.urihttps://hdl.handle.net/10902/36340
dc.description.abstractIn this study, we provide a comprehensive review focused on the NW of the Iberian Peninsula identifying a great amount of research works, including 85 empirical rainfall thresholds for the triggering of landslides, some unpublished to date. While the compiled works provide valuable descriptive insights, the thresholds currently have limited predictive capability. The variety of data and approaches used by different authors complicates the comparison of the results and hinders the development of a global understanding of the study area. However, the statistical comparison of four critical accumulated precipitation-duration datasets for the triggering of landslide events from Gipuzkoa, Cantabria, and Asturias in Spain and the N of Portugal highlights a notable similarity in the critical conditions for rainfall-triggered landslides with durations in the range of 3-12 days. Despite the variety of statistical approaches applied, the unexpected similarity aligns with the homogeneous climatic and orographic characteristics across NW Iberia.es_ES
dc.description.sponsorshipPart of this research has been funded by (1) RETROCLIFF project, call 2021 for Knowledge Generation Projects founded by the Spanish Ministry of Science and Innovation, the Spanish Research Agency (AEI), and the European Regional Development Found (ERDF) [Ref. MCIU-22-PID2021- 122472NB-100], (2) GEOCANTABRICAE project, co-funded by the Foundation for the Promotion of Applied Scientific Research and Technology (FICYT), by the Government of the Principality of Asturias, by the European Union, and by the European Regional Development Found (ERDF) [Ref. SV-PA-21-AYUD/2021/51766], and (3) PAR project “Caracterización de materiales, formas y procesos recientes para mejorar la gestión de los recursos y riesgos geológicos”, University of Cantabria [Ref. 29.P209.64004].es_ES
dc.format.extent27 p.es_ES
dc.language.isoenges_ES
dc.publisherElsevieres_ES
dc.rights© 2025. This manuscript version is made available under the CC-BY-NC-ND 4.0 licensees_ES
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/4.0/
dc.sourceCatena, 2025, 255, 108983es_ES
dc.subject.otherLandslide empirical thresholdes_ES
dc.subject.otherRainfalles_ES
dc.subject.otherPortugales_ES
dc.subject.otherSpaines_ES
dc.titleEmpirical rainfall thresholds for the triggering of landslides in the NW of the Iberian Peninsula: A state of the artes_ES
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.relation.publisherVersionhttps://doi.org/10.1016/j.catena.2025.108983es_ES
dc.rights.accessRightsembargoedAccesses_ES
dc.identifier.DOI10.1016/j.catena.2025.108983
dc.type.versionacceptedVersiones_ES
dc.embargo.lift2027-08-01
dc.date.embargoEndDate2027-08-01


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© 2025. This manuscript version is made available under the CC-BY-NC-ND 4.0 licenseExcepto si se señala otra cosa, la licencia del ítem se describe como © 2025. This manuscript version is made available under the CC-BY-NC-ND 4.0 license