Can Volcanic Dust Suspended From Surface Soil and Deserts of Iceland Be Transferred to Central Balkan Similarly to African Dust (Sahara)?

In 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 Icelandi...

Full description

Bibliographic Details
Published in:Frontiers in Earth Science
Main Authors: Dragana Đorđević, Ivana Tošić, Sanja Sakan, Srđan Petrović, Jelena Đuričić-Milanković, David C. Finger, Pavla Dagsson-Waldhauserová
Format: Article in Journal/Newspaper
Language:English
Published: Frontiers Media S.A. 2019
Subjects:
Online Access:https://doi.org/10.3389/feart.2019.00142
https://doaj.org/article/5887d25025214c61a8645fe8de559a9d
_version_ 1821549317369888768
author Dragana Đorđević
Ivana Tošić
Sanja Sakan
Srđan Petrović
Jelena Đuričić-Milanković
David C. Finger
Pavla Dagsson-Waldhauserová
author_facet Dragana Đorđević
Ivana Tošić
Sanja Sakan
Srđan Petrović
Jelena Đuričić-Milanković
David C. Finger
Pavla Dagsson-Waldhauserová
author_sort Dragana Đorđević
collection Directory of Open Access Journals: DOAJ Articles
container_title Frontiers in Earth Science
container_volume 7
description In 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.
format Article in Journal/Newspaper
genre Iceland
genre_facet Iceland
geographic Rangárvellir
geographic_facet Rangárvellir
id ftdoajarticles:oai:doaj.org/article:5887d25025214c61a8645fe8de559a9d
institution Open Polar
language English
long_lat ENVELOPE(-20.255,-20.255,63.842,63.842)
op_collection_id ftdoajarticles
op_doi https://doi.org/10.3389/feart.2019.00142
op_relation https://www.frontiersin.org/article/10.3389/feart.2019.00142/full
https://doaj.org/toc/2296-6463
2296-6463
doi:10.3389/feart.2019.00142
https://doaj.org/article/5887d25025214c61a8645fe8de559a9d
op_source Frontiers in Earth Science, Vol 7 (2019)
publishDate 2019
publisher Frontiers Media S.A.
record_format openpolar
spelling ftdoajarticles:oai:doaj.org/article:5887d25025214c61a8645fe8de559a9d 2025-01-16T22:32:36+00:00 Can Volcanic Dust Suspended From Surface Soil and Deserts of Iceland Be Transferred to Central Balkan Similarly to African Dust (Sahara)? Dragana Đorđević Ivana Tošić Sanja Sakan Srđan Petrović Jelena Đuričić-Milanković David C. Finger Pavla Dagsson-Waldhauserová 2019-07-01T00:00:00Z https://doi.org/10.3389/feart.2019.00142 https://doaj.org/article/5887d25025214c61a8645fe8de559a9d EN eng Frontiers Media S.A. https://www.frontiersin.org/article/10.3389/feart.2019.00142/full https://doaj.org/toc/2296-6463 2296-6463 doi:10.3389/feart.2019.00142 https://doaj.org/article/5887d25025214c61a8645fe8de559a9d Frontiers in Earth Science, Vol 7 (2019) High Latitude Dust sources backward trajectories chemical fingerprints atmospheric aerosol long-range transport Science Q article 2019 ftdoajarticles https://doi.org/10.3389/feart.2019.00142 2022-12-31T11:56:57Z In 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. Article in Journal/Newspaper Iceland Directory of Open Access Journals: DOAJ Articles Rangárvellir ENVELOPE(-20.255,-20.255,63.842,63.842) Frontiers in Earth Science 7
spellingShingle High Latitude Dust sources
backward trajectories
chemical fingerprints
atmospheric aerosol
long-range transport
Science
Q
Dragana Đorđević
Ivana Tošić
Sanja Sakan
Srđan Petrović
Jelena Đuričić-Milanković
David C. Finger
Pavla Dagsson-Waldhauserová
Can Volcanic Dust Suspended From Surface Soil and Deserts of Iceland Be Transferred to Central Balkan Similarly to African Dust (Sahara)?
title Can Volcanic Dust Suspended From Surface Soil and Deserts of Iceland Be Transferred to Central Balkan Similarly to African Dust (Sahara)?
title_full Can Volcanic Dust Suspended From Surface Soil and Deserts of Iceland Be Transferred to Central Balkan Similarly to African Dust (Sahara)?
title_fullStr Can Volcanic Dust Suspended From Surface Soil and Deserts of Iceland Be Transferred to Central Balkan Similarly to African Dust (Sahara)?
title_full_unstemmed Can Volcanic Dust Suspended From Surface Soil and Deserts of Iceland Be Transferred to Central Balkan Similarly to African Dust (Sahara)?
title_short Can Volcanic Dust Suspended From Surface Soil and Deserts of Iceland Be Transferred to Central Balkan Similarly to African Dust (Sahara)?
title_sort can volcanic dust suspended from surface soil and deserts of iceland be transferred to central balkan similarly to african dust (sahara)?
topic High Latitude Dust sources
backward trajectories
chemical fingerprints
atmospheric aerosol
long-range transport
Science
Q
topic_facet High Latitude Dust sources
backward trajectories
chemical fingerprints
atmospheric aerosol
long-range transport
Science
Q
url https://doi.org/10.3389/feart.2019.00142
https://doaj.org/article/5887d25025214c61a8645fe8de559a9d