Identification and Characterization of Black Carbon Aerosol Sources in the East Baltic Region

One-year continuous measurements of aerosol black carbon (BC) at the background site Preila (55°55′N, 21°00′E, 5 m a.s.l., Lithuania) were performed. Temporal and spatial evolution and transport of biomass burning (BB) and volcanic aerosols observed within this period were explained by the air mass...

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Main Authors: Steigvilė Byčenkienė, Vidmantas Ulevicius, Vadimas Dudoitis, Julija Pauraitė
Format: Article
Language:English
Published: Hindawi Limited 2013-01-01
Series:Advances in Meteorology
Online Access:http://dx.doi.org/10.1155/2013/380614
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spelling doaj-e895ece94f36485db33b0f91738b08082020-11-25T01:09:20ZengHindawi LimitedAdvances in Meteorology1687-93091687-93172013-01-01201310.1155/2013/380614380614Identification and Characterization of Black Carbon Aerosol Sources in the East Baltic RegionSteigvilė Byčenkienė0Vidmantas Ulevicius1Vadimas Dudoitis2Julija Pauraitė3Center for Physical Sciences and Technology, Savanorių 231, LT-02300 Vilnius, LithuaniaCenter for Physical Sciences and Technology, Savanorių 231, LT-02300 Vilnius, LithuaniaCenter for Physical Sciences and Technology, Savanorių 231, LT-02300 Vilnius, LithuaniaCenter for Physical Sciences and Technology, Savanorių 231, LT-02300 Vilnius, LithuaniaOne-year continuous measurements of aerosol black carbon (BC) at the background site Preila (55°55′N, 21°00′E, 5 m a.s.l., Lithuania) were performed. Temporal and spatial evolution and transport of biomass burning (BB) and volcanic aerosols observed within this period were explained by the air mass backward trajectory analysis in conjunction with the fire detection data produced by the MODIS Rapid Response System and AERONET database. The surface measurements and analysis of the Angström exponent of the absorption coefficient done separately for shorter and longer wavelengths (i.e., α=370–520 nm and α=660–950 nm) showed that high levels of aerosol BC were related to the transport of air masses rich in BB products from Ukraine caused by active grass burning. During the events the highest mean values of the Angström exponent of the absorption coefficients α370–520 and α590–950 nm were observed (2.4±0.1 and 1.5±0.1, resp.). The ash plume of the Grimsvötn eruption on May 21, 2011 offered an exceptional opportunity to characterize the volcanic aerosols. The largest ash plume (in terms of aerosol optical thickness) over Lithuania was observed at May 24/25, 2011. The highest values of the Angström exponent of the absorption coefficients α370–520 and α590–950 nm were reached (1.3±0.1 and 1.4±0.1, resp.).http://dx.doi.org/10.1155/2013/380614
collection DOAJ
language English
format Article
sources DOAJ
author Steigvilė Byčenkienė
Vidmantas Ulevicius
Vadimas Dudoitis
Julija Pauraitė
spellingShingle Steigvilė Byčenkienė
Vidmantas Ulevicius
Vadimas Dudoitis
Julija Pauraitė
Identification and Characterization of Black Carbon Aerosol Sources in the East Baltic Region
Advances in Meteorology
author_facet Steigvilė Byčenkienė
Vidmantas Ulevicius
Vadimas Dudoitis
Julija Pauraitė
author_sort Steigvilė Byčenkienė
title Identification and Characterization of Black Carbon Aerosol Sources in the East Baltic Region
title_short Identification and Characterization of Black Carbon Aerosol Sources in the East Baltic Region
title_full Identification and Characterization of Black Carbon Aerosol Sources in the East Baltic Region
title_fullStr Identification and Characterization of Black Carbon Aerosol Sources in the East Baltic Region
title_full_unstemmed Identification and Characterization of Black Carbon Aerosol Sources in the East Baltic Region
title_sort identification and characterization of black carbon aerosol sources in the east baltic region
publisher Hindawi Limited
series Advances in Meteorology
issn 1687-9309
1687-9317
publishDate 2013-01-01
description One-year continuous measurements of aerosol black carbon (BC) at the background site Preila (55°55′N, 21°00′E, 5 m a.s.l., Lithuania) were performed. Temporal and spatial evolution and transport of biomass burning (BB) and volcanic aerosols observed within this period were explained by the air mass backward trajectory analysis in conjunction with the fire detection data produced by the MODIS Rapid Response System and AERONET database. The surface measurements and analysis of the Angström exponent of the absorption coefficient done separately for shorter and longer wavelengths (i.e., α=370–520 nm and α=660–950 nm) showed that high levels of aerosol BC were related to the transport of air masses rich in BB products from Ukraine caused by active grass burning. During the events the highest mean values of the Angström exponent of the absorption coefficients α370–520 and α590–950 nm were observed (2.4±0.1 and 1.5±0.1, resp.). The ash plume of the Grimsvötn eruption on May 21, 2011 offered an exceptional opportunity to characterize the volcanic aerosols. The largest ash plume (in terms of aerosol optical thickness) over Lithuania was observed at May 24/25, 2011. The highest values of the Angström exponent of the absorption coefficients α370–520 and α590–950 nm were reached (1.3±0.1 and 1.4±0.1, resp.).
url http://dx.doi.org/10.1155/2013/380614
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