Vertical and horizontal distribution of regional new particle formation events in Madrid

The vertical profile of new particle formation (NPF) events was studied by comparing the aerosol size number distributions measured aloft and at surface level in a suburban environment in Madrid, Spain, using airborne instruments. The horizontal distribution and regional impact of the NPF events was...

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Autores: Carnerero, Cristina, Pérez, Noemí, Reche, Cristina, Ealo, Marina, Titos, Gloria, Lee, Hong Ku, Eun, Hee Ram, Park, Yonghee, Dada, Lubna, Paasonen, Pauli, Kerminen, Veli Matti, Mantilla, Enrique, Escudero, Miguel, Gómez-Moreno, Francisco Javier, Alonso-Blanco, Elisabeth, Coz, Esther, Saiz-Lopez, A., Temime-Roussel, Brice, Marchand, Nicolas, Beddows, D.C.S., Harrison, Roy M., Petäjä, Tuukka, Kulmala, Markku, Ahn, Kang-Ho, Alastuey, Andrés, Querol, Xavier
Tipo de recurso: artículo
Estado:Versión publicada
Fecha de publicación:2018
País:España
Institución:Consejo Superior de Investigaciones Científicas (CSIC)
Repositorio:DIGITAL.CSIC. Repositorio Institucional del CSIC
OAI Identifier:oai:digital.csic.es:10261/173021
Acceso en línea:http://hdl.handle.net/10261/173021
Access Level:acceso abierto
Palabra clave:New particle formation
NPF
Ultrafine particles
Aerosols
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repository_id_str
dc.title.none.fl_str_mv Vertical and horizontal distribution of regional new particle formation events in Madrid
title Vertical and horizontal distribution of regional new particle formation events in Madrid
spellingShingle Vertical and horizontal distribution of regional new particle formation events in Madrid
Carnerero, Cristina
New particle formation
NPF
Ultrafine particles
Aerosols
title_short Vertical and horizontal distribution of regional new particle formation events in Madrid
title_full Vertical and horizontal distribution of regional new particle formation events in Madrid
title_fullStr Vertical and horizontal distribution of regional new particle formation events in Madrid
title_full_unstemmed Vertical and horizontal distribution of regional new particle formation events in Madrid
title_sort Vertical and horizontal distribution of regional new particle formation events in Madrid
dc.creator.none.fl_str_mv Carnerero, Cristina
Pérez, Noemí
Reche, Cristina
Ealo, Marina
Titos, Gloria
Lee, Hong Ku
Eun, Hee Ram
Park, Yonghee
Dada, Lubna
Paasonen, Pauli
Kerminen, Veli Matti
Mantilla, Enrique
Escudero, Miguel
Gómez-Moreno, Francisco Javier
Alonso-Blanco, Elisabeth
Coz, Esther
Saiz-Lopez, A.
Temime-Roussel, Brice
Marchand, Nicolas
Beddows, D.C.S.
Harrison, Roy M.
Petäjä, Tuukka
Kulmala, Markku
Ahn, Kang-Ho
Alastuey, Andrés
Querol, Xavier
author Carnerero, Cristina
author_facet Carnerero, Cristina
Pérez, Noemí
Reche, Cristina
Ealo, Marina
Titos, Gloria
Lee, Hong Ku
Eun, Hee Ram
Park, Yonghee
Dada, Lubna
Paasonen, Pauli
Kerminen, Veli Matti
Mantilla, Enrique
Escudero, Miguel
Gómez-Moreno, Francisco Javier
Alonso-Blanco, Elisabeth
Coz, Esther
Saiz-Lopez, A.
Temime-Roussel, Brice
Marchand, Nicolas
Beddows, D.C.S.
Harrison, Roy M.
Petäjä, Tuukka
Kulmala, Markku
Ahn, Kang-Ho
Alastuey, Andrés
Querol, Xavier
author_role author
author2 Pérez, Noemí
Reche, Cristina
Ealo, Marina
Titos, Gloria
Lee, Hong Ku
Eun, Hee Ram
Park, Yonghee
Dada, Lubna
Paasonen, Pauli
Kerminen, Veli Matti
Mantilla, Enrique
Escudero, Miguel
Gómez-Moreno, Francisco Javier
Alonso-Blanco, Elisabeth
Coz, Esther
Saiz-Lopez, A.
Temime-Roussel, Brice
Marchand, Nicolas
Beddows, D.C.S.
Harrison, Roy M.
Petäjä, Tuukka
Kulmala, Markku
Ahn, Kang-Ho
Alastuey, Andrés
Querol, Xavier
author2_role author
author
author
author
author
author
author
author
author
author
author
author
author
author
author
author
author
author
author
author
author
author
author
author
author
dc.contributor.none.fl_str_mv European Research Council
Consejo Superior de Investigaciones Científicas [https://ror.org/02gfc7t72]
dc.subject.none.fl_str_mv New particle formation
NPF
Ultrafine particles
Aerosols
topic New particle formation
NPF
Ultrafine particles
Aerosols
description The vertical profile of new particle formation (NPF) events was studied by comparing the aerosol size number distributions measured aloft and at surface level in a suburban environment in Madrid, Spain, using airborne instruments. The horizontal distribution and regional impact of the NPF events was investigated with data from three urban, urban background, and suburban stations in the Madrid metropolitan area. Intensive regional NPF episodes followed by particle growth were simultaneously recorded at three stations in and around Madrid during a field campaign in July 2016. The urban stations presented larger formation rates compared to the suburban station. Condensation and coagulation sinks followed a similar evolution at all stations, with higher values at urban stations. However, the total number concentration of particles larger than 2.5 nm was lower at the urban station and peaked around noon, when black carbon (BC) levels are at a minimum. The vertical soundings demonstrated that ultrafine particles (UFPs) are formed exclusively inside the mixed layer. As convection becomes more effective and the mixed layer grows, UFPs are detected at higher levels. The morning soundings revealed the presence of a residual layer in the upper levels in which aged particles (nucleated and grown on previous days) prevail. The particles in this layer also grow in size, with growth rates significantly smaller than those inside the mixed layer. Under conditions with strong enough convection, the soundings revealed homogeneous number size distributions and growth rates at all altitudes, which follow the same evolution at the other stations considered in this study. This indicates that UFPs are detected quasi-homogenously in an area spanning at least 17 km horizontally. The NPF events extend over the full vertical extension of the mixed layer, which can reach as high as 3000 m in the area, according to previous studies. On some days a marked decline in particle size (shrinkage) was observed in the afternoon, associated with a change in air masses. Additionally, a few nocturnal nucleation-mode bursts were observed at the urban stations, for which further research is needed to elucidate their origin. © Author(s) 2018.
publishDate 2018
dc.date.none.fl_str_mv 2018
2018
2018
dc.type.none.fl_str_mv info:eu-repo/semantics/article
http://purl.org/coar/resource_type/c_6501
Publisher's version
info:eu-repo/semantics/publishedVersion
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status_str publishedVersion
dc.identifier.none.fl_str_mv http://hdl.handle.net/10261/173021
url http://hdl.handle.net/10261/173021
dc.language.none.fl_str_mv Inglés
language_invalid_str_mv Inglés
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info:eu-repo/grantAgreement/EC/H2020/742206
info:eu-repo/grantAgreement/MINECO/Plan Estatal de Investigación Científica y Técnica y de Innovación 2013-2016/CGL2016-78594-R
info:eu-repo/grantAgreement/EC/H2020/689443
https://doi.org/10.5194/acp-18-16601-2018

dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
eu_rights_str_mv openAccess
dc.publisher.none.fl_str_mv Copernicus Publications
publisher.none.fl_str_mv Copernicus Publications
dc.source.none.fl_str_mv reponame:DIGITAL.CSIC. Repositorio Institucional del CSIC
instname:Consejo Superior de Investigaciones Científicas (CSIC)
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reponame_str DIGITAL.CSIC. Repositorio Institucional del CSIC
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spelling Vertical and horizontal distribution of regional new particle formation events in MadridCarnerero, CristinaPérez, NoemíReche, CristinaEalo, MarinaTitos, GloriaLee, Hong KuEun, Hee RamPark, YongheeDada, LubnaPaasonen, PauliKerminen, Veli MattiMantilla, EnriqueEscudero, MiguelGómez-Moreno, Francisco JavierAlonso-Blanco, ElisabethCoz, EstherSaiz-Lopez, A.Temime-Roussel, BriceMarchand, NicolasBeddows, D.C.S.Harrison, Roy M.Petäjä, TuukkaKulmala, MarkkuAhn, Kang-HoAlastuey, AndrésQuerol, XavierNew particle formationNPFUltrafine particlesAerosolsThe vertical profile of new particle formation (NPF) events was studied by comparing the aerosol size number distributions measured aloft and at surface level in a suburban environment in Madrid, Spain, using airborne instruments. The horizontal distribution and regional impact of the NPF events was investigated with data from three urban, urban background, and suburban stations in the Madrid metropolitan area. Intensive regional NPF episodes followed by particle growth were simultaneously recorded at three stations in and around Madrid during a field campaign in July 2016. The urban stations presented larger formation rates compared to the suburban station. Condensation and coagulation sinks followed a similar evolution at all stations, with higher values at urban stations. However, the total number concentration of particles larger than 2.5 nm was lower at the urban station and peaked around noon, when black carbon (BC) levels are at a minimum. The vertical soundings demonstrated that ultrafine particles (UFPs) are formed exclusively inside the mixed layer. As convection becomes more effective and the mixed layer grows, UFPs are detected at higher levels. The morning soundings revealed the presence of a residual layer in the upper levels in which aged particles (nucleated and grown on previous days) prevail. The particles in this layer also grow in size, with growth rates significantly smaller than those inside the mixed layer. Under conditions with strong enough convection, the soundings revealed homogeneous number size distributions and growth rates at all altitudes, which follow the same evolution at the other stations considered in this study. This indicates that UFPs are detected quasi-homogenously in an area spanning at least 17 km horizontally. The NPF events extend over the full vertical extension of the mixed layer, which can reach as high as 3000 m in the area, according to previous studies. On some days a marked decline in particle size (shrinkage) was observed in the afternoon, associated with a change in air masses. Additionally, a few nocturnal nucleation-mode bursts were observed at the urban stations, for which further research is needed to elucidate their origin. © Author(s) 2018.This work was supported by the Spanish Ministry of Agriculture, Fishing, Food and Environment; the Ministry of Economy, Industry and Competitiveness; the Madrid City Council and Regional Government; FEDER funds under the project HOUSE (CGL2016-78594-R); the CUD of Zaragoza (project CUD 2016-05); the Government of Catalonia (AGAUR 2017 SGR44); and the Korean Ministry of Environment through “The Eco-Innovation project”. The funding received by ERA-PLANET (http://www.era-planet.eu, last access: 16 November 2018), the trans-national project SMURBS (http://www.smurbs.eu, last access: 16 November 2018) (Grant agreement No. 689443), and the support of the Academy of Finland via the Center of Excellence in Atmospheric Sciences are acknowledged. These results are part of a project (ATM-GTP/ERC) that has received funding from the European Research Council (ERC) under the European Union’s Horizon 2020 research and innovation program (Grant agreement No. 742206). The authors also acknowledge the Doctoral program of Atmospheric Sciences at the University of Helsinki (ATM-DP). Markku Kulmala acknowledges the support of the Academy of Finland via his Academy Professorship (no. 302958). We also thank the City Council of Majadahonda for logistic assistance, and the Instituto de Ciencias Agrarias, Instituto de Salud Carlos III, Alava Ingenieros, TSI, Solma Environmental Solutions, and Airmodus for their support.Peer reviewedCopernicus PublicationsEuropean Research CouncilConsejo Superior de Investigaciones Científicas [https://ror.org/02gfc7t72]201820182018info:eu-repo/semantics/articlehttp://purl.org/coar/resource_type/c_6501Publisher's versioninfo:eu-repo/semantics/publishedVersionhttp://hdl.handle.net/10261/173021reponame:DIGITAL.CSIC. 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