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dc.contributor.authorRemondo Tejerina, Juan es_ES
dc.contributor.authorBonachea Pico, Jaime es_ES
dc.contributor.authorRivas Mantecón, María Victoria es_ES
dc.contributor.authorSánchez Espeso, Javier María es_ES
dc.contributor.authorBruschi, Viola María es_ES
dc.contributor.authorCendrero Uceda, Antonio es_ES
dc.contributor.authorDíaz de Terán Mira, José Ramón es_ES
dc.contributor.authorFernández Maroto, Gema es_ES
dc.contributor.authorGómez Arozamena, José Ezequiel es_ES
dc.contributor.authorGonzález Díez, Alberto es_ES
dc.contributor.authorSainz Fernández, Carlos es_ES
dc.contributor.otherUniversidad de Cantabriaes_ES
dc.date.accessioned2024-01-15T07:16:40Z
dc.date.available2024-01-15T07:16:40Z
dc.date.issued2017es_ES
dc.identifier.isbn978-3-319-53498-5es_ES
dc.identifier.otherCGL2013-46425-Pes_ES
dc.identifier.urihttps://hdl.handle.net/10902/31084
dc.description.abstractThe goal of this contribution is to develop a set of methods and techniques for modelling landslide hazard, in order to obtain better predictions and, therefore, to reduce the risk associated to this type of process. The research has been carried out in North-Western Guipúzcoa (Spain), an area intensely affected by shallow landslides. Hazard predictions must be based on several assumptions, termed scenarios. To propose more realistic hazard scenarios, two different approaches have been applied: on one hand, by extrapolating the trends observed from recent past landslide activity and, on the other hand and indirectly, from the empirical analyses between landslides and their main trigger (precipitation). It was necessary to get long time series of landslide occurrences, through which sound future frequency could be estimated and relationships between landslides and their predisposing factors established. The landslide inventory includes 20 time intervals ranging from the 50s of last century to the present and has been obtained by analyzing photographic images from different dates. Rainfall records of several weather stations have been analyzed, establishing correlations between landslides and precipitation intensity-duration. According to rainfall quantity, duration and intensity, as well as landslide activity, six multiple occurrence regional landslide events (MORLE), regarding rainfall extreme events, have been identified and characterized. On the basis of both types of scenarios quantitative hazard models could be obtained.
dc.format.extent8 p.es_ES
dc.language.isoenges_ES
dc.rightsAlojado según Resolución CNEAI 5/12/23 (ANECA)es_ES
dc.rights© Springer International Publishing AG 2017
dc.sourceAdvancing Culture of Living with Landslides, Springer International Publishing, 2017es_ES
dc.subject.otherLandslides
dc.subject.otherFrequency
dc.subject.otherRainfall threshold
dc.subject.otherScenarios
dc.subject.otherLandslide hazard and risk
dc.subject.otherGuipúzcoa
dc.titleLandslide hazard scenarios based on both past landslides and precipitationes_ES
dc.typeinfo:eu-repo/semantics/conferenceObjectes_ES
dc.relation.publisherVersionhttps://doi.org/10.1007/978-3-319-53498-5_111es_ES
dc.rights.accessRightsclosedAccess
dc.identifier.DOI10.1007/978-3-319-53498-5_111es_ES
dc.type.versionpublishedVersiones_ES


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