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Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/10470
DC FieldValueLanguage
dc.contributor.authorallJódar, J.en
dc.contributor.authorallCustodio, E.en
dc.contributor.authorallLiotta, M.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italiaen
dc.contributor.authorallLambán, L. J.en
dc.contributor.authorallHerrera, C.en
dc.contributor.authorallMartos-Rosillo, S.en
dc.contributor.authorallSapriza, G.en
dc.contributor.authorallRigo, T.en
dc.date.accessioned2017-03-08T08:57:48Zen
dc.date.available2017-03-08T08:57:48Zen
dc.date.issued2016en
dc.identifier.urihttp://hdl.handle.net/2122/10470en
dc.description.abstractAbstract The time series of stable water isotope composition relative to IAEA-GNIP meteorological stations located in alpine zones are analyzed in order to study how the amplitude of the seasonal isotopic composition of precipitation (Aδ) varies along a vertical transect. A clear relationship between Aδ and local evaporation is obtained, with slopes of â 0.87 â °/100 mm/yr and â 7.3 â °/100 mm/yr for Aδ18O and Aδ2H, respectively. When all sampling points of the vertical transect receive the same moisture sources, then a linear relationship between Aδ and elevation is obtained, with vertical gradients of 0.16 â °/100 mm/yr and 1.46 â °/100 mm/yr for Aδ18O and Aδ2H, respectively.en
dc.language.isoEnglishen
dc.publisher.nameElsevier Science Limiteden
dc.relation.ispartofScience of The Total Environmenten
dc.relation.ispartofseries/550 (2016)en
dc.subjectSeasonal isotopic amplitudeen
dc.titleCorrelation of the seasonal isotopic amplitude of precipitation with annual evaporation and altitude in alpine regionsen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber27-37en
dc.subject.INGV01. Atmosphere::01.01. Atmosphere::01.01.01. Composition and Structureen
dc.identifier.doi10.1016/j.scitotenv.2015.12.034en
dc.description.obiettivoSpecifico6A. Monitoraggio ambientale, sicurezza e territorioen
dc.description.journalTypeJCR Journalen
dc.description.fulltextrestricteden
dc.relation.issn0048-9697en
dc.relation.eissn1879-1026en
dc.contributor.authorJódar, J.en
dc.contributor.authorCustodio, E.en
dc.contributor.authorLiotta, M.en
dc.contributor.authorLambán, L. J.en
dc.contributor.authorHerrera, C.en
dc.contributor.authorMartos-Rosillo, S.en
dc.contributor.authorSapriza, G.en
dc.contributor.authorRigo, T.en
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italiaen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextembargo_restricted_21010101-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Palermo, Palermo, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Palermo, Palermo, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Palermo, Palermo, Italia-
crisitem.author.orcid0000-0002-7203-1565-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent01. Atmosphere-
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