Geochemistry of PM10 over Europe during the EMEP intensive measurement periods in summer 2012 and winter 2013
The third intensive measurement period (IMP) organised by the European Monitoring and Evaluation Programme (EMEP) under the UNECE CLTRAP took place in summer 2012 and winter 2013, with PM10 filter samples concurrently collected at 20 (16 EMEP) regional background sites across Europe for subsequent analysis of their mineral dust content. All samples were analysed by the same or a comparable methodology. Higher PM10 mineral dust loadings were observed at most sites in summer (0.5-10 μgm-3) compared to winter (0.2-2 μgm-3), with the most elevated concentrations in the southern-and easternmost countries, accounting for 20-40% of PM10. Saharan dust outbreaks were responsible for the high summer dust loadings at western and central European sites, whereas regional or local sources explained the elevated concentrations observed at eastern sites. The eastern Mediterranean sites experienced elevated levels due to African dust outbreaks during both summer and winter. The mineral dust composition varied more in winter than in summer, with a higher relative contribution of anthropogenic dust during the former period. A relatively high contribution of K from non-mineral and non-sea-salt sources, such as biomass burning, was evident in winter at some of the central and eastern European sites. The spatial distribution of some components and metals reveals the influence of specific anthropogenic sources on a regional scale: shipping emissions (V, Ni, and SO2- 4 ) in the Mediterranean region, metallurgy (Cr, Ni, and Mn) in central and eastern Europe, high temperature processes (As, Pb, and SO2- 4 ) in eastern countries, and traffic (Cu) at sites affected by emissions from nearby cities. © 2016 Author(s). CC Attribution 3.0 License.
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Language: | English |
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European Geosciences Union
2016-03-19
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Subjects: | Mineral dust, Geochemistry, PM10, EMEP, |
Online Access: | http://hdl.handle.net/10261/136473 http://dx.doi.org/10.13039/501100000780 |
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Mineral dust Geochemistry PM10 EMEP Mineral dust Geochemistry PM10 EMEP |
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Mineral dust Geochemistry PM10 EMEP Mineral dust Geochemistry PM10 EMEP Alastuey, Andrés Querol, Xavier Aas, Wenche Lucarelli, Franco Perez, Noemi Moreno, Teresa Cavalli, Fabrizia Areskoug, Hans Balan, Violeta Catrambone, Maria Ceburnis, Darius Cerro, José Carlos Conil, Sébastien Gevorgyan, Lusine Hueglin, Christoph Imre, Kornélia Jaffrezo, Jean Luc Leeson, Sarah R. Mihalopoulos, Nikolaos Mitošinková, Marta O.'Dowd, Colin D. Pey, Jorge Putaud, Jean-Philippe Riffault, Véronique Ripoll, Anna Sciare, Jean Sellegri, Karine Spindler, Gerald Yttri, Karl Espen Geochemistry of PM10 over Europe during the EMEP intensive measurement periods in summer 2012 and winter 2013 |
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The third intensive measurement period (IMP) organised by the European Monitoring and Evaluation Programme (EMEP) under the UNECE CLTRAP took place in summer 2012 and winter 2013, with PM10 filter samples concurrently collected at 20 (16 EMEP) regional background sites across Europe for subsequent analysis of their mineral dust content. All samples were analysed by the same or a comparable methodology. Higher PM10 mineral dust loadings were observed at most sites in summer (0.5-10 μgm-3) compared to winter (0.2-2 μgm-3), with the most elevated concentrations in the southern-and easternmost countries, accounting for 20-40% of PM10. Saharan dust outbreaks were responsible for the high summer dust loadings at western and central European sites, whereas regional or local sources explained the elevated concentrations observed at eastern sites. The eastern Mediterranean sites experienced elevated levels due to African dust outbreaks during both summer and winter. The mineral dust composition varied more in winter than in summer, with a higher relative contribution of anthropogenic dust during the former period. A relatively high contribution of K from non-mineral and non-sea-salt sources, such as biomass burning, was evident in winter at some of the central and eastern European sites. The spatial distribution of some components and metals reveals the influence of specific anthropogenic sources on a regional scale: shipping emissions (V, Ni, and SO2- 4 ) in the Mediterranean region, metallurgy (Cr, Ni, and Mn) in central and eastern Europe, high temperature processes (As, Pb, and SO2- 4 ) in eastern countries, and traffic (Cu) at sites affected by emissions from nearby cities. © 2016 Author(s). CC Attribution 3.0 License. |
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European Commission |
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European Commission Alastuey, Andrés Querol, Xavier Aas, Wenche Lucarelli, Franco Perez, Noemi Moreno, Teresa Cavalli, Fabrizia Areskoug, Hans Balan, Violeta Catrambone, Maria Ceburnis, Darius Cerro, José Carlos Conil, Sébastien Gevorgyan, Lusine Hueglin, Christoph Imre, Kornélia Jaffrezo, Jean Luc Leeson, Sarah R. Mihalopoulos, Nikolaos Mitošinková, Marta O.'Dowd, Colin D. Pey, Jorge Putaud, Jean-Philippe Riffault, Véronique Ripoll, Anna Sciare, Jean Sellegri, Karine Spindler, Gerald Yttri, Karl Espen |
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artículo |
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Mineral dust Geochemistry PM10 EMEP |
author |
Alastuey, Andrés Querol, Xavier Aas, Wenche Lucarelli, Franco Perez, Noemi Moreno, Teresa Cavalli, Fabrizia Areskoug, Hans Balan, Violeta Catrambone, Maria Ceburnis, Darius Cerro, José Carlos Conil, Sébastien Gevorgyan, Lusine Hueglin, Christoph Imre, Kornélia Jaffrezo, Jean Luc Leeson, Sarah R. Mihalopoulos, Nikolaos Mitošinková, Marta O.'Dowd, Colin D. Pey, Jorge Putaud, Jean-Philippe Riffault, Véronique Ripoll, Anna Sciare, Jean Sellegri, Karine Spindler, Gerald Yttri, Karl Espen |
author_sort |
Alastuey, Andrés |
title |
Geochemistry of PM10 over Europe during the EMEP intensive measurement periods in summer 2012 and winter 2013 |
title_short |
Geochemistry of PM10 over Europe during the EMEP intensive measurement periods in summer 2012 and winter 2013 |
title_full |
Geochemistry of PM10 over Europe during the EMEP intensive measurement periods in summer 2012 and winter 2013 |
title_fullStr |
Geochemistry of PM10 over Europe during the EMEP intensive measurement periods in summer 2012 and winter 2013 |
title_full_unstemmed |
Geochemistry of PM10 over Europe during the EMEP intensive measurement periods in summer 2012 and winter 2013 |
title_sort |
geochemistry of pm10 over europe during the emep intensive measurement periods in summer 2012 and winter 2013 |
publisher |
European Geosciences Union |
publishDate |
2016-03-19 |
url |
http://hdl.handle.net/10261/136473 http://dx.doi.org/10.13039/501100000780 |
work_keys_str_mv |
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dig-idaea-es-10261-1364732022-10-11T10:22:59Z Geochemistry of PM10 over Europe during the EMEP intensive measurement periods in summer 2012 and winter 2013 Alastuey, Andrés Querol, Xavier Aas, Wenche Lucarelli, Franco Perez, Noemi Moreno, Teresa Cavalli, Fabrizia Areskoug, Hans Balan, Violeta Catrambone, Maria Ceburnis, Darius Cerro, José Carlos Conil, Sébastien Gevorgyan, Lusine Hueglin, Christoph Imre, Kornélia Jaffrezo, Jean Luc Leeson, Sarah R. Mihalopoulos, Nikolaos Mitošinková, Marta O.'Dowd, Colin D. Pey, Jorge Putaud, Jean-Philippe Riffault, Véronique Ripoll, Anna Sciare, Jean Sellegri, Karine Spindler, Gerald Yttri, Karl Espen European Commission Mineral dust Geochemistry PM10 EMEP The third intensive measurement period (IMP) organised by the European Monitoring and Evaluation Programme (EMEP) under the UNECE CLTRAP took place in summer 2012 and winter 2013, with PM10 filter samples concurrently collected at 20 (16 EMEP) regional background sites across Europe for subsequent analysis of their mineral dust content. All samples were analysed by the same or a comparable methodology. Higher PM10 mineral dust loadings were observed at most sites in summer (0.5-10 μgm-3) compared to winter (0.2-2 μgm-3), with the most elevated concentrations in the southern-and easternmost countries, accounting for 20-40% of PM10. Saharan dust outbreaks were responsible for the high summer dust loadings at western and central European sites, whereas regional or local sources explained the elevated concentrations observed at eastern sites. The eastern Mediterranean sites experienced elevated levels due to African dust outbreaks during both summer and winter. The mineral dust composition varied more in winter than in summer, with a higher relative contribution of anthropogenic dust during the former period. A relatively high contribution of K from non-mineral and non-sea-salt sources, such as biomass burning, was evident in winter at some of the central and eastern European sites. The spatial distribution of some components and metals reveals the influence of specific anthropogenic sources on a regional scale: shipping emissions (V, Ni, and SO2- 4 ) in the Mediterranean region, metallurgy (Cr, Ni, and Mn) in central and eastern Europe, high temperature processes (As, Pb, and SO2- 4 ) in eastern countries, and traffic (Cu) at sites affected by emissions from nearby cities. © 2016 Author(s). CC Attribution 3.0 License. The present work was supported by the Cooperative Programme for Monitoring and Evaluation of the Longrange Transmission of Air pollutants in Europe (EMEP) under UNECE. We also acknowledge support by the European Union Seventh Framework Programme (FP7/2007-2013) through ACTRIS (grant agreement no. 262254) and by the European Union’s Horizon 2020 research and innovation programme under grant agreement No. 654109. The participation of IDAEA-CSIC was supported by the Spanish Ministry of Economy and Competitiveness and FEDER funds under the project PRISMA (CGL2012-39623-C02-1), by the Generalitat de Catalunya (AGAUR 2015 SGR33 and the DGQA). The authors wish to thank the Norwegian Ministry of foreign affairs for support to the measurements in Armenia and Moldova. The French participation to the campaigns was funded by the French Agency of Environment and Energy Management (ADEME, grants 1262C0022 and 1262C0039). Mines Douai acknowledges support from the CaPPA project which is financed by the French National Research Agency (ANR) through the PIA (Programme d’Investissement d’Avenir) under contract ANR-11-LABX-0005- 01, the “Nord-Pas de Calais” Regional Council and the European Regional Development Fund (ERDF). Participation of the ANDRA is also acknowledged for the measurements at OPE-ANDRA. The authors are also indebted to the fieldwork teams at Auchencorth Moss and Harwell (NERC CEH and Riccardo Energy and Environment Staff). The authors would also like to express our gratitude to the Atmospheric Modelling Laboratory from the Barcelona Supercomputing Centre, the Naval Research Laboratory and the SeaWiFS project (NASA) for the provision of the DREAM, NAAPs aerosol maps and the satellite imagery, respectively. The authors wish to thank D. C. Carslaw and K. Ropkins for providing the Openair software used in this paper (Carslaw and Ropkins, 2012; Carslaw, 2012). Peer reviewed 2016-09-08T07:21:15Z 2016-09-08T07:21:15Z 2016-03-19 artículo http://purl.org/coar/resource_type/c_6501 Atmospheric Chemistry and Physics 161 (10): 6107-6129 (2016) http://hdl.handle.net/10261/136473 10.5194/acp-16-6107-2016 http://dx.doi.org/10.13039/501100000780 en #PLACEHOLDER_PARENT_METADATA_VALUE# info:eu-repo/grantAgreement/EC/FP7/262254 http://dx.doi.org/10.5194/acp-16-6107-2016 Sí open European Geosciences Union |