Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/16255
DC FieldValueLanguage
dc.date.accessioned2023-02-28T06:53:08Z-
dc.date.available2023-02-28T06:53:08Z-
dc.date.issued2022-03-
dc.identifier.urihttp://hdl.handle.net/2122/16255-
dc.description.abstractHazardous ground deformation and landslides occur frequently in the Mila Basin, Algeria and this problem remains unsolved. However, the historical seismicity in the area indicates no severe damage from past earthquakes. For this reason, studies are needed to monitor the slow ground movements and their triggering factors. Since about two decades ago, satellite observations by interferometric synthetic aperture radar (InSAR) technique and the multi-temporal (MT-InSAR) technique have provided a tool for monitoring slow and extremely slow ground displacements. In this study, 2D decomposition of InSAR outputs revealed a sliding surface at two regions located 12 km apart, indicating slow motion rather than fast movement along the damaged area. We concluded that the factors leading to surface displacement in the investigated area include the triggering earthquakes, precipitation, terrain topography and soil moisture. This study contributes to landslide hazard identification and risk assessment in the Mila Basin.en_US
dc.language.isoEnglishen_US
dc.publisher.nameWileyen_US
dc.relation.ispartofTerra Novaen_US
dc.relation.ispartofseries/34 (2022)en_US
dc.rightsAttribution-NonCommercial-NoDerivs 3.0 United States*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/us/*
dc.subjectLandslidesen_US
dc.subjectInSARen_US
dc.subjectAlgeriaen_US
dc.subjectHazarden_US
dc.subjectLandslide monitoring using MT-InSAR technique in Algeriaen_US
dc.titleMulti‐temporal InSAR analysis to monitor landslides using the small baseline subset (SBAS) approach in the Mila Basin, Algeriaen_US
dc.typearticleen
dc.description.statusPublisheden_US
dc.type.QualityControlPeer-revieweden_US
dc.description.pagenumber407–423en_US
dc.identifier.doi10.1111/ter.12591en_US
dc.description.obiettivoSpecifico2T. Deformazione crostale attivaen_US
dc.description.journalTypeJCR Journalen_US
dc.relation.issn0954-4879en_US
dc.contributor.authorMedhat, Noha Ismail-
dc.contributor.authorYamamoto, Masa‐yuki-
dc.contributor.authorTolomei, Cristiano-
dc.contributor.authorHarbi, Assia-
dc.contributor.authorMaouche, Said-
dc.contributor.departmentNational Research Institute of Astronomy and Geophysics, Cairo, Helwan, Egypten_US
dc.contributor.departmentSchool of Systems Engineering, Kochi University of Technology, Kami, Kochi, Japanen_US
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italiaen_US
dc.contributor.departmentCentre de Recherche en Astronomie, Astrophysique et Géophysique, Algiers, Algeriaen_US
dc.contributor.departmentCentre de Recherche en Astronomie, Astrophysique et Géophysique, Algiers, Algeriaen_US
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextopen-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptNational Research Institute of Astronomy and Geophysics, Cairo, Helwan, Egypt-
crisitem.author.deptSchool of Systems Engineering, Kochi University of Technology, Kami, Kochi, Japan-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia-
crisitem.author.orcid0000-0001-7378-0712-
crisitem.author.orcid0000-0002-3867-3329-
crisitem.author.orcid0000-0002-5925-8028-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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