Please use this identifier to cite or link to this item: http://hdl.handle.net/10553/130636
DC FieldValueLanguage
dc.contributor.authorValdivielso, Soniaen_US
dc.contributor.authorMurray, Jesicaen_US
dc.contributor.authorCustodio Gimena, Emilioen_US
dc.contributor.authorHassanzadeh, Ashkanen_US
dc.contributor.authorMartinez, Daniel Emilioen_US
dc.contributor.authorVazquez-Sune, Enricen_US
dc.date.accessioned2024-05-23T09:57:01Z-
dc.date.available2024-05-23T09:57:01Z-
dc.date.issued2024en_US
dc.identifier.issn0048-9697en_US
dc.identifier.otherWoS-
dc.identifier.urihttp://hdl.handle.net/10553/130636-
dc.description.abstractPrecipitation plays a crucial role in the natural hydrological cycle. Understanding the spatial and temporal variations of precipitation isotopes is essential for identifying hydrological, meteorological, and ecological processes. In high mountain areas with arid and semi-arid conditions, especially in regions with endorheic basins, the portion of precipitation that infiltrates the groundwater as the primary source of water recharge. However, estimating this recharge is challenging and prone to high uncertainty. The main objective of this study was to implement a robust and detailed methodology to analyze the influence of meteorological variables and the origin of moisture sources on the stable isotopic composition (8 18 O and 8 2 H) of precipitation. As an illustrative case, we focused on the Los Pozuelos Basin, an endorheic basin in the Altiplano-Puna region of the Andes. The analysis incorporated precipitation samples collected over a 3-year period (January 2020 to April 2023) along with comprehensive monitoring of local atmospheric variables, satellite imagery, and HYSPLIT backward trajectory models. The examination involved a multivariate analysis of meteorological and stable isotope data and atmospheric transport pattern. Precipitation characteristics exhibited seasonal variability, with summer precipitation being depleted in heavy isotopes due to its extended continental journey and the recycling it undergoes while crossing the Amazon basin with convective activity. Another moisture path from the Atlantic Ocean, via the Rio de la Plata or Gran Chaco basin, represented an intermediate isotopic stage. La Nin a events intensified westerly winds, drawing moist air masses from the Pacific Ocean and causing rainfall in the study area. In winter, precipitation comes from the Pacific Ocean and isotopically enriched due to the low amount of precipitation and lower convective activity. By employing a meticulous methodology and multivariate statistical analysis, the study contributes positively to the broader discourse on water resource management and conservation in arid and semi -arid environments.en_US
dc.languagespaen_US
dc.relation.ispartofScience of the Total Environmenten_US
dc.sourceScience Of The Total Environment [ISSN 0048-9697], v. 925,en_US
dc.subject2502 Climatologíaen_US
dc.subject.otherStable-Isotopesen_US
dc.subject.otherCentral Andesen_US
dc.subject.otherVariance Testen_US
dc.subject.otherDelta-O-18en_US
dc.subject.otherClimateen_US
dc.subject.otherWateren_US
dc.subject.otherVariabilityen_US
dc.subject.otherGroundwateren_US
dc.subject.otherEnsoen_US
dc.subject.otherEvaporationen_US
dc.subject.otherLos Pozuelos Basinen_US
dc.subject.otherStable Isotopesen_US
dc.subject.otherBack Trajectoriesen_US
dc.subject.otherHyspliten_US
dc.subject.otherOlren_US
dc.subject.otherConvectiveen_US
dc.titleSeasonal and isotopic precipitation patterns in the semi-arid and high mountain areasen_US
dc.typeinfo:eu-repo/semantics/Articleen_US
dc.typeArticleen_US
dc.identifier.doi10.1016/j.scitotenv.2024.171750en_US
dc.identifier.isi001215436600001-
dc.identifier.eissn1879-1026-
dc.relation.volume925en_US
dc.investigacionArtes y Humanidadesen_US
dc.type2Artículoen_US
dc.contributor.daisngidNo ID-
dc.contributor.daisngidNo ID-
dc.contributor.daisngidNo ID-
dc.contributor.daisngidNo ID-
dc.contributor.daisngidNo ID-
dc.contributor.daisngidNo ID-
dc.description.numberofpages14en_US
dc.utils.revisionen_US
dc.contributor.wosstandardWOS:Valdivielso, S-
dc.contributor.wosstandardWOS:Murray, J-
dc.contributor.wosstandardWOS:Custodio, E-
dc.contributor.wosstandardWOS:Hassanzadeh, A-
dc.contributor.wosstandardWOS:Martínez, DE-
dc.contributor.wosstandardWOS:Vazquez-Suñé, E-
dc.date.coverdateMayo 2024en_US
dc.identifier.ulpgcen_US
dc.contributor.buulpgcBU-HUMen_US
dc.description.sjr1,998
dc.description.jcr9,8
dc.description.sjrqQ1
dc.description.jcrqQ1
dc.description.scieSCIE
dc.description.miaricds11,0
item.fulltextSin texto completo-
item.grantfulltextnone-
crisitem.author.deptGIR IUNAT: Geología de Terrenos Volcánicos-
crisitem.author.deptIU de Estudios Ambientales y Recursos Naturales-
crisitem.author.orcid0000-0003-4122-8098-
crisitem.author.parentorgIU de Estudios Ambientales y Recursos Naturales-
crisitem.author.fullNameCustodio Gimena,Emilio-
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