A case study on biomass burning aerosols: effects on aerosol optical properties and surface radiation levels

In spring 2006, biomass burning aerosols from eastern Europe were transported extensively to Finland, and to other parts of northern Europe. They were observed as far as in the European Arctic. In the first part of this paper, temporal and spatial evolution and transport of these biomass burning aer...

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Published in:Atmospheric Chemistry and Physics
Main Authors: Arola, A., Lindfors, A., Natunen, A., Lehtinen, K. E. J.
Format: Text
Language:English
Published: 2018
Subjects:
Online Access:https://doi.org/10.5194/acp-7-4257-2007
https://www.atmos-chem-phys.net/7/4257/2007/
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spelling ftcopernicus:oai:publications.copernicus.org:acp4674 2023-05-15T15:09:38+02:00 A case study on biomass burning aerosols: effects on aerosol optical properties and surface radiation levels Arola, A. Lindfors, A. Natunen, A. Lehtinen, K. E. J. 2018-01-15 application/pdf https://doi.org/10.5194/acp-7-4257-2007 https://www.atmos-chem-phys.net/7/4257/2007/ eng eng doi:10.5194/acp-7-4257-2007 https://www.atmos-chem-phys.net/7/4257/2007/ eISSN: 1680-7324 Text 2018 ftcopernicus https://doi.org/10.5194/acp-7-4257-2007 2019-12-24T09:58:32Z In spring 2006, biomass burning aerosols from eastern Europe were transported extensively to Finland, and to other parts of northern Europe. They were observed as far as in the European Arctic. In the first part of this paper, temporal and spatial evolution and transport of these biomass burning aerosols are monitored with MODIS retrieved aerosol optical depth (AOD) imagery at visible wavelengths (0.55 μm). Comparison of MODIS and AERONET AOD is conducted at Tõravere, Estonia. Then trajectory analyses, as well as MODIS Fire Mapper products are used to better understand the type and origin of the air masses. During the studied four-week period AOD values ranged from near zero up to 1.2 at 0.55 μm and the linear correlation between MODIS and AERONET was very high (~0.97). Temporal variability observed within this four-week period was also rather well explained by the trajectory analysis in conjunction with the fire detections produced by the MODIS Rapid Response System. In the second part of our study, the surface measurements of global and UV radiation at Jokioinen, Finland are used to study the effect of this haze episode on the levels of surface radiation. We found reductions up to 35% in noon-time surface UV irradiance (at 340 nm) as compared to typical aerosol conditions. For global (total solar) radiation, the reduction was always smaller, in line with the expected wavelength dependence of the aerosol effect. Text Arctic Copernicus Publications: E-Journals Arctic Atmospheric Chemistry and Physics 7 16 4257 4266
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language English
description In spring 2006, biomass burning aerosols from eastern Europe were transported extensively to Finland, and to other parts of northern Europe. They were observed as far as in the European Arctic. In the first part of this paper, temporal and spatial evolution and transport of these biomass burning aerosols are monitored with MODIS retrieved aerosol optical depth (AOD) imagery at visible wavelengths (0.55 μm). Comparison of MODIS and AERONET AOD is conducted at Tõravere, Estonia. Then trajectory analyses, as well as MODIS Fire Mapper products are used to better understand the type and origin of the air masses. During the studied four-week period AOD values ranged from near zero up to 1.2 at 0.55 μm and the linear correlation between MODIS and AERONET was very high (~0.97). Temporal variability observed within this four-week period was also rather well explained by the trajectory analysis in conjunction with the fire detections produced by the MODIS Rapid Response System. In the second part of our study, the surface measurements of global and UV radiation at Jokioinen, Finland are used to study the effect of this haze episode on the levels of surface radiation. We found reductions up to 35% in noon-time surface UV irradiance (at 340 nm) as compared to typical aerosol conditions. For global (total solar) radiation, the reduction was always smaller, in line with the expected wavelength dependence of the aerosol effect.
format Text
author Arola, A.
Lindfors, A.
Natunen, A.
Lehtinen, K. E. J.
spellingShingle Arola, A.
Lindfors, A.
Natunen, A.
Lehtinen, K. E. J.
A case study on biomass burning aerosols: effects on aerosol optical properties and surface radiation levels
author_facet Arola, A.
Lindfors, A.
Natunen, A.
Lehtinen, K. E. J.
author_sort Arola, A.
title A case study on biomass burning aerosols: effects on aerosol optical properties and surface radiation levels
title_short A case study on biomass burning aerosols: effects on aerosol optical properties and surface radiation levels
title_full A case study on biomass burning aerosols: effects on aerosol optical properties and surface radiation levels
title_fullStr A case study on biomass burning aerosols: effects on aerosol optical properties and surface radiation levels
title_full_unstemmed A case study on biomass burning aerosols: effects on aerosol optical properties and surface radiation levels
title_sort case study on biomass burning aerosols: effects on aerosol optical properties and surface radiation levels
publishDate 2018
url https://doi.org/10.5194/acp-7-4257-2007
https://www.atmos-chem-phys.net/7/4257/2007/
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op_relation doi:10.5194/acp-7-4257-2007
https://www.atmos-chem-phys.net/7/4257/2007/
op_doi https://doi.org/10.5194/acp-7-4257-2007
container_title Atmospheric Chemistry and Physics
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