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Shallow and deep landslides induced by rainfall in the Lisbon region (Portugal): assessment of relationships with the North Atlantic oscillation

dc.contributor.authorZêzere, José
dc.contributor.authorTrigo, R. M.
dc.contributor.authorTrigo, I. F.
dc.date.accessioned2019-02-14T16:32:06Z
dc.date.available2019-02-14T16:32:06Z
dc.date.issued2005
dc.description.abstractThe aim of this study is to assess the impact of the North Atlantic Oscillation (NAO) on both the winter precipitation and the temporal occurrence of different landslide types in Portugal. The analysis is applied to five sample areas located just north of Lisbon, the capital of Portugal. These sites are particularly relevant because actual dates of most of the recent landslide events are known but also because the landslides occurred in a suburban area with growing urbanization pressure. Results show that the large inter-annual variability of winter precipitation observed in western Iberia, i.e. Portugal and parts of Spain, is largely modulated by the NAO mode. In particular, precipitation falling in Portugal between November and March presents a correlation coefficient of R=–0.66 with the NAO index. Precipitation distribution for the reference rain gauge in the study area reveals that the probability of a wet month to occur is much higher for low NAO index composites than for the corresponding high NAO index composite. It is shown that this control, exerted by NAO on the precipitation regime, is related to corresponding changes in the associated activity of North-Atlantic storm tracks that affect the western Iberia. Landslide activity in the study area is related to both intense, short duration precipitation events (1–15 days) and long-lasting rainfall episodes (1–3 months). The former events trigger shallow translational slides while the later episodes are usually associated with deeper and larger slope movements. This second group of landslides is shown to be statistically associated with the 3-month average of the NAO index.pt_PT
dc.description.versioninfo:eu-repo/semantics/publishedVersionpt_PT
dc.identifier.citationZezere, J. L., Trigo, R. M., & Trigo, I. F. (2005). Shallow and deep landslides induced by rainfall in the Lisbon region (Portugal): assessment of relationships with the North Atlantic oscillation. Natural Hazards and Earth System Sciences, 5(3), 331–344. https://doi.org/10.5194/nhess-5-331-2005pt_PT
dc.identifier.doi10.5194/nhess-5-331-2005pt_PT
dc.identifier.issn1561-8633
dc.identifier.issn1684-9981
dc.identifier.urihttp://hdl.handle.net/10451/37012
dc.language.isoengpt_PT
dc.peerreviewedyespt_PT
dc.publisherCopernicus Publicationspt_PT
dc.relation.publisherversionhttps://www.nat-hazards-earth-syst-sci.net/5/331/2005/nhess-5-331-2005.pdfpt_PT
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/pt_PT
dc.subjectLandslidespt_PT
dc.subjectDebris flowspt_PT
dc.subjectNorth Atlantic Oscillationpt_PT
dc.subjectRainfallpt_PT
dc.subjectLisbonpt_PT
dc.subjectPortugalpt_PT
dc.titleShallow and deep landslides induced by rainfall in the Lisbon region (Portugal): assessment of relationships with the North Atlantic oscillationpt_PT
dc.typejournal article
dspace.entity.typePublication
oaire.citation.endPage344pt_PT
oaire.citation.issue3pt_PT
oaire.citation.startPage331pt_PT
oaire.citation.titleNatural Hazards and Earth System Sciencespt_PT
oaire.citation.volume5pt_PT
person.familyNameZêzere
person.givenNameJosé Luís
person.identifierH-9956-2013
person.identifier.ciencia-id511D-EE6B-47E3
person.identifier.orcid0000-0002-3953-673X
person.identifier.scopus-author-id6507109389
rcaap.rightsopenAccesspt_PT
rcaap.typearticlept_PT
relation.isAuthorOfPublicationa49d5ad5-533a-4973-b8c6-a4f201b1cf62
relation.isAuthorOfPublication.latestForDiscoverya49d5ad5-533a-4973-b8c6-a4f201b1cf62

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