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dc.contributor.authorReyes Carmona, Cristina 
dc.contributor.authorGalve Arnedo, Jorge Pedro 
dc.contributor.authorPérez Peña, José Vicente 
dc.contributor.authorMoreno Sánchez, Marcos
dc.contributor.authorJorde, David Alfonso
dc.contributor.authorBallesteros Posada, Daniel 
dc.contributor.authorTorre, Davide
dc.contributor.authorAzañón Hernández, José Miguel 
dc.contributor.authorMateos, Rosa María
dc.date.accessioned2023-06-16T08:31:44Z
dc.date.available2023-06-16T08:31:44Z
dc.date.issued2023-05-26
dc.identifier.citationReyes-Carmona, C., Galve, J.P., Pérez-Peña, J.V. et al. Improving landslide inventories by combining satellite interferometry and landscape analysis: the case of Sierra Nevada (Southern Spain). Landslides (2023). [https://doi.org/10.1007/s10346-023-02071-1]es_ES
dc.identifier.urihttps://hdl.handle.net/10481/82530
dc.description.abstractAn updated and complete landslide inventory is the starting point for an appropriate hazard assessment. This paper presents an improvement for landslide mapping by integrating data from two well-consolidated techniques: Differential Synthetic Aperture Radar (DInSAR) and Landscape Analysis through the normalised channel steepness index (ksn). The southwestern sector of the Sierra Nevada mountain range (Southern Spain) was selected as the case study. We first propose the double normalised steepness (ksnn) index, derived from the ksn index, to remove the active tectonics signal. The obtained ksnn anomalies (or knickzones) along rivers and the unstable ground areas from the DInSAR analysis rapidly highlighted the slopes of interest. Thus, we provided a new inventory of 28 landslides that implies an increase in the area affected by landslides compared with the previous mapping: 33.5% in the present study vs. 14.5% in the Spanish Land Movements Database. The two main typologies of identified landslides are Deep-Seated Gravitational Slope Deformations (DGSDs) and rockslides, with the prevalence of large DGSDs in Sierra Nevada being first revealed in this work. We also demonstrate that the combination of DInSAR and Landscape Analysis could overcome the limitations of each method for landslide detection. They also supported us in dealing with difficulties in recognising this type of landslides due to their poorly defined boundaries, a homogeneous lithology and the imprint of glacial and periglacial processes. Finally, a preliminary hazard perspective of these landslides was outlined.es_ES
dc.description.sponsorshipUniversidad de Granada/CBUAes_ES
dc.description.sponsorshipMarie Curie Actions B-RNM-305-UGR18 A-RNM-508-UGR20 P18-RT-3632es_ES
dc.description.sponsorshipERDF through the project RISKCOAST' of the Interreg SUDOE Programme SOE3/P4/E0868es_ES
dc.description.sponsorshipProject MORPHOMED' from the Spanish Ministry of Science (MCIN)/State Research Agency (SRA) PID2019-107138RB-I00es_ES
dc.description.sponsorshipRamon y Cajal' Programme of the Spanish Ministry of Science RYC-2017-23335es_ES
dc.description.sponsorshipNoR 63737es_ES
dc.language.isoenges_ES
dc.publisherSpringerNaturees_ES
dc.rightsAtribución 4.0 Internacional*
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/*
dc.subjectDInSARes_ES
dc.subjectksnes_ES
dc.subjectLandslide inventoryes_ES
dc.subjectDGSDes_ES
dc.subjectRockslidees_ES
dc.subjectMountain rangees_ES
dc.subjectSierra Nevada es_ES
dc.subjectSouthern Spaines_ES
dc.titleImproving landslide inventories by combining satellite interferometry and landscape analysis: the case of Sierra Nevada (Southern Spain)es_ES
dc.typejournal articlees_ES
dc.rights.accessRightsopen accesses_ES
dc.identifier.doi10.1007/s10346-023-02071-1
dc.type.hasVersionVoRes_ES


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