Identificador persistente para citar o vincular este elemento: http://hdl.handle.net/10553/52314
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dc.contributor.authorCana-Cascallar, Luis C.en_US
dc.contributor.otherCana-Cascallar, Luis-
dc.date.accessioned2018-11-25T19:15:10Z-
dc.date.available2018-11-25T19:15:10Z-
dc.date.issued2002en_US
dc.identifier.issn1096-2247en_US
dc.identifier.urihttp://hdl.handle.net/10553/52314-
dc.description.abstractSpanish European Monitoring and Evaluation Programme (EMEP) stations were selected to relate acid rain episodes with the meteorological structure that caused the rainfall during a 5-year period. A principal component analysis (PCA) was used to determine the origin of major ions (SO4 2−, NO3 −, Cl−, Ca2+, K+, Mg2+, and Na+) in the rainwater. In addition, the meteorological origin of the rain was identified. Previous works suggested a relationship between acid rain and storm convective clouds. However, statistical analyses of pH values show that only the short-lived con-vective phenomena may cause acid rain in Spain. In fact, rain generated by fronts and that related to long-lived convective systems is neutral or even slightly basic. Results suggest that the acid rain might be related to the meteorological time scale instead of to the cloud type.en_US
dc.languageengen_US
dc.publisher1096-2247
dc.relation.ispartofJournal of the Air and Waste Management Associationen_US
dc.sourceJournal of the Air and Waste Management Association [ISSN 1096-2247], v. 52, p. 334-338en_US
dc.subject2502 Climatologíaen_US
dc.subject.otherAcid rainen_US
dc.subject.otherEnvironmental monitoringen_US
dc.subject.otherHydrogen-ion concentrationen_US
dc.subject.otherSpainen_US
dc.titleOn the relationship between acid rain and cloud typeen_US
dc.typeinfo:eu-repo/semantics/Articleen_US
dc.typeArticleen_US
dc.identifier.doi10.1080/10473289.2002.10470785
dc.identifier.scopus0036119896-
dc.identifier.isi000174330000011-
dcterms.isPartOfJournal Of The Air & Waste Management Association
dcterms.sourceJournal Of The Air & Waste Management Association[ISSN 1047-3289],v. 52 (3), p. 334-338
dc.contributor.authorscopusid8153672300-
dc.description.lastpage338en_US
dc.description.firstpage334en_US
dc.relation.volume52en_US
dc.investigacionCienciasen_US
dc.type2Artículoen_US
dc.identifier.wosWOS:000174330000011-
dc.contributor.daisngid4176723-
dc.identifier.investigatorRIDA-7663-2008-
dc.utils.revisionen_US
dc.contributor.wosstandardWOS:Cana-Cascallar, LC
dc.date.coverdateEnero 2002
dc.identifier.ulpgces
dc.description.sellofecytSello FECYT
dc.description.scieSCIE
item.grantfulltextnone-
item.fulltextSin texto completo-
crisitem.author.deptGIR IOCAG: Oceanografía Física-
crisitem.author.deptIU de Oceanografía y Cambio Global-
crisitem.author.deptDepartamento de Física-
crisitem.author.orcid0000-0001-6006-5488-
crisitem.author.parentorgIU de Oceanografía y Cambio Global-
crisitem.author.fullNameCana Cascallar, Luis Cesáreo-
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