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dc.contributor.authorChen, Gang
dc.contributor.authorCanonaco, Francesco
dc.contributor.authorTobler, Anna
dc.contributor.authorAas, Wenche
dc.contributor.authorAlastuey, Andres
dc.contributor.authorAllan, James
dc.contributor.authorAtabakhsh, Samira
dc.contributor.authorAurela, Minna
dc.contributor.authorBaltensperger, Urs
dc.contributor.authorBougiatioti, Aikaterini
dc.contributor.authorDe Brito, Joel F.
dc.contributor.authorCeburnis, Darius
dc.contributor.authorChazeau, Benjamin
dc.contributor.authorChebaicheb, Hasna
dc.contributor.authorDaellenbach, Kaspar R.
dc.contributor.authorEhn, Mikael
dc.contributor.authorEl Haddad, Imad
dc.contributor.authorEleftheriadis, Konstantinos
dc.contributor.authorFavez, Olivier
dc.contributor.authorFlentje, Harald
dc.contributor.authorFont, Anna
dc.contributor.authorFossum, Kirsten
dc.contributor.authorFreney, Evelyn
dc.contributor.authorGini, Maria
dc.contributor.authorGreen, David C
dc.contributor.authorHeikkinen, Liine
dc.contributor.authorHerrmann, Hartmut
dc.contributor.authorKalogridis, Athina-Cerise
dc.contributor.authorKeernik, Hannes
dc.contributor.authorLhotka, Radek
dc.contributor.authorLin, Chunshui
dc.contributor.authorLunder, Chris Rene
dc.contributor.authorMaasikmets, Marek
dc.contributor.authorManousakas, Manousos I.
dc.contributor.authorMarchand, Nicolas
dc.contributor.authorMarin, Cristina
dc.contributor.authorMarmureanu, Luminita
dc.contributor.authorMihalopoulos, Nikolaos
dc.contributor.authorMočnik, Griša
dc.contributor.authorNęcki, Jaroslaw
dc.contributor.authorO'Dowd, Colin
dc.contributor.authorOvadnevaite, Jurgita
dc.contributor.authorPeter, Thomas
dc.contributor.authorPetit, Jean-Eudes
dc.contributor.authorPikridas, Michael
dc.contributor.authorPlatt, Stephen Matthew
dc.contributor.authorPokorná, Petra
dc.contributor.authorPoulain, Laurent
dc.contributor.authorPriestman, Max
dc.contributor.authorRiffault, Véronique
dc.contributor.authorRinaldi, Matteo
dc.contributor.authorRóżański, Kazimierz
dc.contributor.authorSchwarz, Jaroslav
dc.contributor.authorSciare, Jean
dc.contributor.authorSimon, Leïla
dc.contributor.authorSkiba, Alicja
dc.contributor.authorSlowik, Jay G.
dc.contributor.authorSosedova, Yulia
dc.contributor.authorStavroulas, Iasonas
dc.contributor.authorStyszko, Katarzyna
dc.contributor.authorTeinemaa, Erik
dc.contributor.authorTimonen, Hilkka
dc.contributor.authorTremper, Anja
dc.contributor.authorVasilescu, Jeni
dc.contributor.authorVia, Marta
dc.contributor.authorVodička, Petr
dc.contributor.authorWiedensohler, Alfred
dc.contributor.authorZografou, Olga
dc.contributor.authorCruz Minguillón, María
dc.contributor.authorPrévôt, André S.H.
dc.date.accessioned2022-09-27T06:52:02Z
dc.date.available2022-09-27T06:52:02Z
dc.date.created2022-09-02T11:24:44Z
dc.date.issued2022
dc.identifier.citationEnvironment International. 2022, 166, 107325.en_US
dc.identifier.issn0160-4120
dc.identifier.urihttps://hdl.handle.net/11250/3021583
dc.description.abstractOrganic aerosol (OA) is a key component of total submicron particulate matter (PM1), and comprehensive knowledge of OA sources across Europe is crucial to mitigate PM1 levels. Europe has a well-established air quality research infrastructure from which yearlong datasets using 21 aerosol chemical speciation monitors (ACSMs) and 1 aerosol mass spectrometer (AMS) were gathered during 2013–2019. It includes 9 non-urban and 13 urban sites. This study developed a state-of-the-art source apportionment protocol to analyse long-term OA mass spectrum data by applying the most advanced source apportionment strategies (i.e., rolling PMF, ME-2, and bootstrap). This harmonised protocol was followed strictly for all 22 datasets, making the source apportionment results more comparable. In addition, it enables quantification of the most common OA components such as hydrocarbon-like OA (HOA), biomass burning OA (BBOA), cooking-like OA (COA), more oxidised-oxygenated OA (MO-OOA), and less oxidised-oxygenated OA (LO-OOA). Other components such as coal combustion OA (CCOA), solid fuel OA (SFOA: mainly mixture of coal and peat combustion), cigarette smoke OA (CSOA), sea salt (mostly inorganic but part of the OA mass spectrum), coffee OA, and ship industry OA could also be separated at a few specific sites. Oxygenated OA (OOA) components make up most of the submicron OA mass (average = 71.1%, range from 43.7 to 100%). Solid fuel combustion-related OA components (i.e., BBOA, CCOA, and SFOA) are still considerable with in total 16.0% yearly contribution to the OA, yet mainly during winter months (21.4%). Overall, this comprehensive protocol works effectively across all sites governed by different sources and generates robust and consistent source apportionment results. Our work presents a comprehensive overview of OA sources in Europe with a unique combination of high time resolution (30–240 min) and long-term data coverage (9–36 months), providing essential information to improve/validate air quality, health impact, and climate models.en_US
dc.language.isoengen_US
dc.rightsNavngivelse 4.0 Internasjonal*
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no*
dc.titleEuropean aerosol phenomenology − 8: Harmonised source apportionment of organic aerosol using 22 Year-long ACSM/AMS datasetsen_US
dc.typePeer revieweden_US
dc.typeJournal articleen_US
dc.description.versionpublishedVersionen_US
dc.rights.holder© 2022 The Authors. Published by Elsevier Ltd.en_US
dc.source.pagenumber18en_US
dc.source.volume166en_US
dc.source.journalEnvironment Internationalen_US
dc.identifier.doi10.1016/j.envint.2022.107325
dc.identifier.cristin2048235
dc.relation.projectNILU - Norsk institutt for luftforskning: 7726en_US
dc.relation.projectNILU - Norsk institutt for luftforskning: 121005en_US
dc.source.articlenumber107325en_US
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode1


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