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dc.creatorĐorđević, Dragana
dc.creatorTošić, Ivana
dc.creatorSakan, Sanja
dc.creatorPetrović, Srđan
dc.creatorĐuričić - Milanković, Jelena
dc.creatorFinger, David Christian
dc.creatorDagsson-Waldhauserová, Pavla
dc.date.accessioned2020-11-26T14:01:06Z
dc.date.available2020-11-26T14:01:06Z
dc.date.issued2019
dc.identifier.issn2296-6463
dc.identifier.urihttps://cer.ihtm.bg.ac.rs/handle/123456789/3859
dc.description.abstractIn this work we use chemical fingerprints as characteristics ratios of specific crustal elements Ca/Al, Fe/Al, K/Al, Mg/Al, Mn/Al, Ca/Fe, and Mg/Fe to investigate the long-range transport of volcanic aerosols from Iceland. Volcanic dust enters the atmosphere during suspension processes from Icelandic deserts, but mainly from the dust hot spots in remote areas in Iceland, and it is transmitted to the central Balkan area (Belgrade). For this purpose, backward trajectories from Belgrade (φ = 44°48′; λ = 20°28′) in 2012 and 2013, simultaneous with atmospheric aerosols measurements, were calculated by using the Hybrid Single-Particle Lagrangian Integrated Trajectory (HYSPLIT) model. We found that about 17% of air masses passed over Icelandic territory and arrived to Balkan area. In almost all of these episodes ratios of some investigated elements in suburban aerosols of Balkan area corresponded to the ratios of elements investigated in surface soil of the Rangárvellir area – South Iceland in the vicinity of volcanoes. We identified several episodes, such as August 6–8, 2012; June 2–6, 2013; June 26–28, 2013; and September 18–20, 2013; with the characteristic ratios of the highest number of investigated elements in atmospheric aerosol of central Balkan corresponding to ratios from Icelandic soil material. This study provides evidence that Icelandic dust can travel long distances showing the importance of High Latitude Dust sources. © 2019 Đorđević, Tošić, Sakan, Petrović, Đuričić-Milanković, Finger and Dagsson-Waldhauserová.en
dc.language.isoensr
dc.publisherSwitzerland : Frontiers Media S.A.sr
dc.relationinfo:eu-repo/grantAgreement/MESTD/Basic Research (BR or ON)/172001/RS//sr
dc.relationinfo:eu-repo/grantAgreement/MESTD/Basic Research (BR or ON)/176013/RS//sr
dc.relationinfo:eu-repo/grantAgreement/MESTD/Integrated and Interdisciplinary Research (IIR or III)/43007/RS//sr
dc.relationIcelandic Research Fund (Rannis) 152248-051sr
dc.relationCOST-STSM-ES1306-34336sr
dc.rightsopenAccesssr
dc.sourceFrontiers in Earth Sciencesr
dc.subjectAtmospheric aerosolsr
dc.subjectBackward trajectoriessr
dc.subjectChemical fingerprintssr
dc.subjectHigh Latitude Dust sourcessr
dc.subjectLong-range transportsr
dc.titleCan volcanic dust suspended from surface soil and deserts of Iceland be transferred to central Balkan similarly to African dust (Sahara)?en
dc.typearticlesr
dc.rights.licenseBYsr
dcterms.abstractТошић, Ивана; Дагссон-Wалдхаусеровá, Павла; Фингер, Давид Ц.; Ђуричић - Миланковић, Јелена; Петровић, Срђан; Сакан, Сања; Ђорђевић, Драгана;
dc.rights.holderThe Authorssr
dc.citation.volume7
dc.citation.spage142
dc.citation.rankM21
dc.identifier.doi10.3389/feart.2019.00142
dc.identifier.fulltexthttp://cer.ihtm.bg.ac.rs/bitstream/id/17968/-or-evi-_et_al-2019-Frontiers_in_Earth_Science.pdf
dc.identifier.scopus2-s2.0-85068468460
dc.identifier.wos000473757200001
dc.type.versionpublishedVersionsr


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