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dc.contributor.authorLange, Benjamin A.
dc.contributor.authorSalganik, Evgenii
dc.contributor.authorMacfarlane, Amy
dc.contributor.authorSchneebeli, Martin
dc.contributor.authorHøyland, Knut Vilhelm
dc.contributor.authorGardner, Jessie
dc.contributor.authorMüller, Oliver
dc.contributor.authorDivine, Dmitry
dc.contributor.authorKohlbach, Doreen
dc.contributor.authorKatlein, Christian
dc.contributor.authorGranskog, Mats
dc.date.accessioned2023-08-18T11:08:58Z
dc.date.available2023-08-18T11:08:58Z
dc.date.issued2023-05-29
dc.description.abstractAn assessment of potential groundwater areas in the Ifni basin, located in the western AntiAtlas range of Morocco, was conducted based on a multicriteria analytical approach that integrated a set of geomorphological and hydroclimatic factors influencing the availability of this resource. This approach involved the use of geographic information systems (GIS) and hierarchical analytical process (AHP) models. Different factors were classified and weighted according to their contribution to and impact on groundwater reserves. Their normalized weights were evaluated using a pairwise comparison matrix. Four classes of potentiality emerged: very high, high, moderate, and low, occupying 15.22%, 20.17%, 30.96%, and 33.65%, respectively, of the basin’s area. A groundwater potential map (GWPA) was validated by comparison with data from 134 existing water points using a receiver operating characteristic (ROC) curve. The AUC was calculated at 80%, indicating the good predictive accuracy of the AHP method. These results will enable water operators to select favorable sites with a high groundwater potential.en_US
dc.identifier.citationLange, Salganik, Macfarlane, Schneebeli, Høyland, Gardner, Müller, Divine, Kohlbach, Katlein, Granskog. Snowmelt contribution to Arctic first-year ice ridge mass balance and rapid consolidation during summer melt. Elementa: Science of the Anthropocene. 2023;11(1)en_US
dc.identifier.cristinIDFRIDAID 2151132
dc.identifier.doi10.1525/elementa.2022.00037
dc.identifier.issn2325-1026
dc.identifier.urihttps://hdl.handle.net/10037/30087
dc.language.isoengen_US
dc.publisherUniversity of California Pressen_US
dc.relation.journalElementa: Science of the Anthropocene
dc.relation.projectIDinfo:eu-repo/grantAgreement/EC/H2020/730965/EU/Arctic Research Icebreaker Consortium: A strategy for meeting the needs for marine-based research in the Arctic/ARICE/en_US
dc.rights.accessRightsopenAccessen_US
dc.rights.holderCopyright 2023 The Author(s)en_US
dc.rights.urihttps://creativecommons.org/licenses/by/4.0en_US
dc.rightsAttribution 4.0 International (CC BY 4.0)en_US
dc.subjectVDP::Matematikk og naturvitenskap: 400::Geofag: 450::Andre geofag: 469en_US
dc.subjectVDP::Mathematics and natural scienses: 400::Geosciences: 450::Other geosciences: 469en_US
dc.subjectPolhavet / Arctic oceanen_US
dc.subjectSea ice geophysics / Sea ice geophysicsen_US
dc.subjectSjøis / Sea iceen_US
dc.subjectSmelting / Meltingen_US
dc.subjectSnø / Snowen_US
dc.titleSnowmelt contribution to Arctic first-year ice ridge mass balance and rapid consolidation during summer melten_US
dc.type.versionpublishedVersionen_US
dc.typeJournal articleen_US
dc.typeTidsskriftartikkelen_US
dc.typePeer revieweden_US


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Attribution 4.0 International (CC BY 4.0)
Except where otherwise noted, this item's license is described as Attribution 4.0 International (CC BY 4.0)