Please use this identifier to cite or link to this item: https://physrep.ff.bg.ac.rs/handle/123456789/1135
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dc.contributor.authorMiljević, Nadaen
dc.contributor.authorPešić, Anaen
dc.contributor.authorGolobočanin, Dušanen
dc.contributor.authorGršić, Zoranen
dc.contributor.authorUnkašević, Miroslavaen
dc.contributor.authorTošić, Ivanaen
dc.date.accessioned2022-07-12T18:19:37Z-
dc.date.available2022-07-12T18:19:37Z-
dc.date.issued2011-12-01en
dc.identifier.issn1788-2281en
dc.identifier.urihttps://physrep.ff.bg.ac.rs/handle/123456789/1135-
dc.description.abstractDaily precipitation was collected in the period from May to December 2010, along with the corresponding meteorological data (air temperature, humidity, amount of precipitation) in the Vinca Institute of Nuclear Sciences (44°45′33″ ″N, 20°35′57″ ″E), Belgrade, Serbia. On the basis of backward trajectory analysis, three dominant trajectory categories are determined: southwestern Europe (SW), northeastern Europe (NE), and northwestern Europe (NW), which were associated with 49 (71%) of the events. The highest daily δ18O and δ2H values were measured on 9 December (-1.3 and-8.7, respectively), whereas the lowest values were measured on 28 December (-143.2% and-19.3%, respectively). Circulation back trajectories, synoptic-scale surface and middle-tropospheric weather maps, and δ2H and δ2O values for 69 precipitation samples, were examined to determine the origin and direction of the air masses for each event.en
dc.relation.ispartofCentral European Geologyen
dc.subjectBelgradeen
dc.subjectdaily precipitationen
dc.subjectstable isotope contenten
dc.titleRelationship between atmospheric circulation and stable isotope composition of Belgrade daily precipitationen
dc.typeArticleen
dc.identifier.doi10.1556/CEuGeol.53.2010.4.5en
dc.identifier.scopus2-s2.0-84855661849en
dc.identifier.urlhttps://api.elsevier.com/content/abstract/scopus_id/84855661849en
dc.relation.issue4en
dc.relation.volume53en
dc.relation.firstpage419en
dc.relation.lastpage422en
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.grantfulltextnone-
item.cerifentitytypePublications-
item.openairetypeArticle-
item.fulltextNo Fulltext-
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