Integration of measurements and model simulations to characterize Eyjafjallajökull volcanic aerosols over south-eastern Italy

Volcanic aerosols resulting from the Eyjafjallajökull eruption were detected in south-eastern Italy from 20 to 22 April 2010, at a distance of approximately 4000 km from the volcano, and have been characterized by lidar, sun/sky photometer, and surface in-situ measurements. Volcanic particles added...

Full description

Bibliographic Details
Published in:Atmospheric Chemistry and Physics
Main Authors: Perrone, M. R., Tomasi, F., Stohl, A., Kristiansen, N. I.
Format: Text
Language:English
Published: 2018
Subjects:
Online Access:https://doi.org/10.5194/acp-12-10001-2012
https://www.atmos-chem-phys.net/12/10001/2012/
id ftcopernicus:oai:publications.copernicus.org:acp15671
record_format openpolar
spelling ftcopernicus:oai:publications.copernicus.org:acp15671 2023-05-15T16:09:29+02:00 Integration of measurements and model simulations to characterize Eyjafjallajökull volcanic aerosols over south-eastern Italy Perrone, M. R. Tomasi, F. Stohl, A. Kristiansen, N. I. 2018-01-15 application/pdf https://doi.org/10.5194/acp-12-10001-2012 https://www.atmos-chem-phys.net/12/10001/2012/ eng eng doi:10.5194/acp-12-10001-2012 https://www.atmos-chem-phys.net/12/10001/2012/ eISSN: 1680-7324 Text 2018 ftcopernicus https://doi.org/10.5194/acp-12-10001-2012 2019-12-24T09:55:46Z Volcanic aerosols resulting from the Eyjafjallajökull eruption were detected in south-eastern Italy from 20 to 22 April 2010, at a distance of approximately 4000 km from the volcano, and have been characterized by lidar, sun/sky photometer, and surface in-situ measurements. Volcanic particles added to the pre-existing aerosol load and measurement data allow quantifying the impact of volcanic particles on the aerosol vertical distribution, lidar ratios, the aerosol size distribution, and the ground-level particulate-matter concentrations. Lidar measurements reveal that backscatter coefficients by volcanic particles were about one order of magnitude smaller over south-eastern Italy than over Central Europe. Mean lidar ratios at 355 nm were equal to 64 ± 5 sr inside the volcanic aerosol layer and were characterized by smaller values (47 ± 2 sr) in the underlying layer on 20 April, 19:30 UTC. Lidar ratios and their dependence with the height reduced in the following days, mainly because of the variability of the volcanic particle contributions. Size distributions from sun/sky photometer measurements reveal the presence of volcanic particles with radii r > 0.5 μm on 21 April and that the contribution of coarse volcanic particles increased from 20 to 22 April. The aerosol fine mode fraction from sun/sky photometer measurements varied between values of 0.85 and 0.94 on 20 April and decreased to values between 0.25 and 0.82 on 22 April. Surface measurements of particle size distributions were in good accordance with column averaged particle size distributions from sun/sky photometer measurements. PM 1 /PM 2.5 mass concentration ratios of 0.69, 0.66, and 0.60 on 20, 21, and 22 April, respectively, support the increase of super-micron particles at ground. Measurements from the Regional Air Quality Agency show that PM 10 mass concentrations on 20, 21, and 22 April 2010 were enhanced in the entire Apulia Region. More specifically, PM 10 mass concentrations have on average increased over Apulia Region 22%, 50%, and 28% on 20, 21, and 22 April, respectively, compared to values on 19 April. Finally, the comparison of measurement data with numerical simulations by the FLEXPART dispersion model demonstrates the ability of FLEXPART to model the advection of the volcanic ash over the 4000 km from the Eyjafjallajökull volcano to Southern Italy. Text Eyjafjallajökull Copernicus Publications: E-Journals Atmospheric Chemistry and Physics 12 20 10001 10013
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description Volcanic aerosols resulting from the Eyjafjallajökull eruption were detected in south-eastern Italy from 20 to 22 April 2010, at a distance of approximately 4000 km from the volcano, and have been characterized by lidar, sun/sky photometer, and surface in-situ measurements. Volcanic particles added to the pre-existing aerosol load and measurement data allow quantifying the impact of volcanic particles on the aerosol vertical distribution, lidar ratios, the aerosol size distribution, and the ground-level particulate-matter concentrations. Lidar measurements reveal that backscatter coefficients by volcanic particles were about one order of magnitude smaller over south-eastern Italy than over Central Europe. Mean lidar ratios at 355 nm were equal to 64 ± 5 sr inside the volcanic aerosol layer and were characterized by smaller values (47 ± 2 sr) in the underlying layer on 20 April, 19:30 UTC. Lidar ratios and their dependence with the height reduced in the following days, mainly because of the variability of the volcanic particle contributions. Size distributions from sun/sky photometer measurements reveal the presence of volcanic particles with radii r > 0.5 μm on 21 April and that the contribution of coarse volcanic particles increased from 20 to 22 April. The aerosol fine mode fraction from sun/sky photometer measurements varied between values of 0.85 and 0.94 on 20 April and decreased to values between 0.25 and 0.82 on 22 April. Surface measurements of particle size distributions were in good accordance with column averaged particle size distributions from sun/sky photometer measurements. PM 1 /PM 2.5 mass concentration ratios of 0.69, 0.66, and 0.60 on 20, 21, and 22 April, respectively, support the increase of super-micron particles at ground. Measurements from the Regional Air Quality Agency show that PM 10 mass concentrations on 20, 21, and 22 April 2010 were enhanced in the entire Apulia Region. More specifically, PM 10 mass concentrations have on average increased over Apulia Region 22%, 50%, and 28% on 20, 21, and 22 April, respectively, compared to values on 19 April. Finally, the comparison of measurement data with numerical simulations by the FLEXPART dispersion model demonstrates the ability of FLEXPART to model the advection of the volcanic ash over the 4000 km from the Eyjafjallajökull volcano to Southern Italy.
format Text
author Perrone, M. R.
Tomasi, F.
Stohl, A.
Kristiansen, N. I.
spellingShingle Perrone, M. R.
Tomasi, F.
Stohl, A.
Kristiansen, N. I.
Integration of measurements and model simulations to characterize Eyjafjallajökull volcanic aerosols over south-eastern Italy
author_facet Perrone, M. R.
Tomasi, F.
Stohl, A.
Kristiansen, N. I.
author_sort Perrone, M. R.
title Integration of measurements and model simulations to characterize Eyjafjallajökull volcanic aerosols over south-eastern Italy
title_short Integration of measurements and model simulations to characterize Eyjafjallajökull volcanic aerosols over south-eastern Italy
title_full Integration of measurements and model simulations to characterize Eyjafjallajökull volcanic aerosols over south-eastern Italy
title_fullStr Integration of measurements and model simulations to characterize Eyjafjallajökull volcanic aerosols over south-eastern Italy
title_full_unstemmed Integration of measurements and model simulations to characterize Eyjafjallajökull volcanic aerosols over south-eastern Italy
title_sort integration of measurements and model simulations to characterize eyjafjallajökull volcanic aerosols over south-eastern italy
publishDate 2018
url https://doi.org/10.5194/acp-12-10001-2012
https://www.atmos-chem-phys.net/12/10001/2012/
genre Eyjafjallajökull
genre_facet Eyjafjallajökull
op_source eISSN: 1680-7324
op_relation doi:10.5194/acp-12-10001-2012
https://www.atmos-chem-phys.net/12/10001/2012/
op_doi https://doi.org/10.5194/acp-12-10001-2012
container_title Atmospheric Chemistry and Physics
container_volume 12
container_issue 20
container_start_page 10001
op_container_end_page 10013
_version_ 1766405370943635456