Improving landslide inventories by combining satellite interferometry and landscape analysis: the case of Sierra Nevada (Southern Spain)
Metadatos
Afficher la notice complèteAuteur
Reyes Carmona, Cristina; Galve Arnedo, Jorge Pedro; Pérez Peña, José Vicente; Moreno Sánchez, Marcos; Jorde, David Alfonso; Ballesteros Posada, Daniel; Torre, Davide; Azañón Hernández, José Miguel; Mateos, Rosa MaríaEditorial
SpringerNature
Materia
DInSAR ksn Landslide inventory DGSD Rockslide Mountain range Sierra Nevada Southern Spain
Date
2023-05-26Referencia bibliográfica
Reyes-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]
Patrocinador
Universidad de Granada/CBUA; Marie Curie Actions B-RNM-305-UGR18 A-RNM-508-UGR20 P18-RT-3632; ERDF through the project RISKCOAST' of the Interreg SUDOE Programme SOE3/P4/E0868; Project MORPHOMED' from the Spanish Ministry of Science (MCIN)/State Research Agency (SRA) PID2019-107138RB-I00; Ramon y Cajal' Programme of the Spanish Ministry of Science RYC-2017-23335; NoR 63737Résumé
An 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.