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dc.contributor.authorPandolfi, Marcoes_ES
dc.contributor.authorAlastuey, Andréses_ES
dc.contributor.authorQuerol, Xavieres_ES
dc.contributor.authorGonzález Jiménez, José Luises_ES
dc.contributor.authorJorba, Oriol C.es_ES
dc.contributor.authorOrtega, Amber M.es_ES
dc.contributor.authorBaldasano, José Maríaes_ES
dc.contributor.authorMinguillón, María Cruzes_ES
dc.contributor.authorArtíñano, Begoñaes_ES
dc.contributor.authorSeco, Rogeres_ES
dc.contributor.authorPeñuelas, Josepes_ES
dc.contributor.authorLorente, Jerónimoes_ES
dc.contributor.authorPey, Jorgees_ES
dc.date.accessioned2015-09-30T07:12:02Z-
dc.date.available2015-09-30T07:12:02Z-
dc.date.issued2014-04-27-
dc.identifier.citationJournal of Geophysical Research Atmosphereses_ES
dc.identifier.urihttp://hdl.handle.net/10261/122810-
dc.description.abstractDAURE (Determination of the Sources of Atmospheric Aerosols in Urban and Rural Environments in the Western Mediterranean) was a multidisciplinary international field campaign aimed at investigating the sources and meteorological controls of particulate matter in the Western Mediterranean Basin (WMB). Measurements were simultaneously performed at an urban-coastal (Barcelona, BCN) and a rural-elevated (Montseny, MSY) site pair in NE Spain during winter and summer. State-of-the-art methods such as 14C analysis, proton-transfer reaction mass spectrometry, and high-resolution aerosol mass spectrometry were applied for the first time in the WMB as part of DAURE. WMB regional pollution episodes were associated with high concentrations of inorganic and organic species formed during the transport to inland areas and built up at regional scales. Winter pollutants accumulation depended on the degree of regional stagnation of an air mass under anticyclonic conditions and the planetary boundary layer height. In summer, regional recirculation and biogenic secondary organic aerosols (SOA) formation mainly determined the regional pollutant concentrations. The contribution from fossil sources to organic carbon (OC) and elemental carbon (EC) and hydrocarbon-like organic aerosol concentrations were higher at BCN compared with MSY due to traffic emissions. The relative contribution of nonfossil OC was higher at MSY especially in summer due to biogenic emissions. The fossil OC/EC ratio at MSY was twice the corresponding ratio at BCN indicating that a substantial fraction of fossil OC was due to fossil SOA. In winter, BCN cooking emissions were identified as an important source of modern carbon in primary organic aerosol. Key Points Analysis of the sources and meteorological controls of PM in the WMB.es_ES
dc.description.sponsorshipThis work is supported by the MINECO (Spanish Ministry of Economy and Competitiveness), the MAGRAMA (Spanish Ministry of Agriculture, Food Environment), and FEDER funds; by the Acción Complementaria DAURE CGL2007-30502-E/CLI, the VAMOS project CGL2010-19464/CLI, the European Union (EUSAAR RII3-CT-2006-026140, EUCAARI), and the Departament de Medi Ambient i Habitatge of the Generalitat de Catalunya. This work was partially funded by Generalitat de Catalunya 2009 SGR8D. J. Baldasano and O. Jorba were partly supported by grants CGL2010/19652, CSD2007-0050, and SEV-2011-00067 of Severo Ochoa Program, awarded by the Spanish Government. M.C.Minguillónwas supported by a postdoctoral grant in the frame of Programa Nacional de Movilidad de Recursos Humanos del Plan nacional de I-D+ I 2008–2011 from the Spanish Ministry of Science and Innovation and by the JAE-Doc CSIC program, cofunded by the European Social Fund (ESF). M. Pandolfi was funded by the Jae-DOC CSIC program cofunded by the European Social Fund (ESF). A. Day, A. M. Ortega, and J. L. Jimenez were partially supported by U.S. NSF grants ATM-0920940 and ATM- 0919189 (from Atm. Chem. and OISE – Office of International Science and Engineering), and by DOE grant DESC0006035. A.M. Ortega was supported by DOE SCGF (ARRA/ORISE/ORAU) Fellowship DE-AC05-06OR23100; J. Peñuelas and R. Seco were supported by the Spanish Government projects CGL2010-17172 and Consolider Ingenio Montes CSD2008-00040, by the Catalan Government project SGR2009-458, and by a postdoctoral grant from Fundación Ramón Areces to R. Seco. Lidar measurements were supported by the 7th Framework Programme project Aerosols, Clouds, and Trace Gases Research Infrastructure Network (ACTRIS) (grant agreement 262254); by the Spanish Ministry of Science and Innovation and FEDER funds under the projects TEC2012- 34575, TEC2009-09106/TEC, CGL2011- 13580-E/CLI, and CGL2011-16124-E/CLI. Also acknowledged is L. Wacker (ETH Zurich) for making available the accelerator mass spectrometer MICADAS for 14C measurement. The authors would also like to acknowledge NASA/Goddard Space Flight Center, SeaWIFS-NASA Project, University of Athens, Navy Research Laboratory-USA, and the Barcelona Supercomputing Centre for their contribution with TOMS maps, satellite images, SKIRON dust maps, NAAPs aerosol maps, and BSC-DREAM8b dust maps, respectively. The authors gratefully acknowledge the NOAA Air Resources Laboratory (ARL) for the provision of the HYSPLIT transport and dispersion model and/or READY website (http://www.arl.noaa.gov/ready.html)es_ES
dc.language.isoenges_ES
dc.publisherAmerican Geophysical Uniones_ES
dc.relationinfo:eu-repo/grantAgreement /EC/FP7/654109es_ES
dc.relation.isversionofPublisher's versiones_ES
dc.rightsopenAccesses_ES
dc.subjectbiogenic SOAes_ES
dc.subjectDAUREes_ES
dc.subjectfossil OC and EC sourceses_ES
dc.subjectinorganic saltses_ES
dc.subjectpollution episodees_ES
dc.subjectWestern Mediterranean Basines_ES
dc.titleEffects of sources and meteorology on particulate matter in the Western Mediterranean Basin: An overview of the DAURE campaignes_ES
dc.typeArtículoes_ES
dc.identifier.doi10.1002/2013JD021079-
dc.description.peerreviewedPeer reviewedes_ES
dc.relation.publisherversion10.1002/2013JD021079es_ES
dc.contributor.funderEuropean Commissiones_ES
dc.relation.csices_ES
dc.identifier.funderhttp://dx.doi.org/10.13039/501100000780es_ES
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