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Primary Versus Secondary Contributions to Particle Number Concentrations in the European Boundary Layer
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SYSNO ASEP 0372230 Document Type J - Journal Article R&D Document Type Journal Article Subsidiary J Článek ve WOS Title Primary Versus Secondary Contributions to Particle Number Concentrations in the European Boundary Layer Author(s) Reddington, C.L. (GB)
Carslaw, K.S. (GB)
Spracklen, D.V. (GB)
Frontoso, M.G. (CH)
Collins, L. (GB)
Merikanto, J. (GB)
Minikin, A. (DE)
Hamburger, T. (DE)
Coe, H. (GB)
Kulmala, M. (FI)
Aalto, P. (FI)
Flentje, H. (DE)
Plass-Dülmer, C. (DE)
Birmili, W. (DE)
Wiedensohler, A. (DE)
Wehner, B. (DE)
Tuch, T. (DE)
Sonntag, A. (DE)
O'Dowd, C.D. (IE)
Jennings, S.G. (IE)
Dupuy, R. (IE)
Baltensperger, U. (CH)
Weingartner, A. (CH)
Hansson, H.-C. (SE)
Tunved, P. (SE)
Laj, P. (FR)
Sellegri, K. (FR)
Boulon, J. (FR)
Putaund, J.-P. (IT)
Gruening, C. (IT)
Swietlicki, E. (SE)
Roldin, P. (SE)
Henzing, J.S. (NL)
Moerman, M. (NL)
Mihalopoulos, N. (GR)
Kouvarakis, G. (GR)
Ždímal, Vladimír (UCHP-M) RID, ORCID, SAI
Zíková, Naděžda (UCHP-M) RID, ORCID, SAI
Marinoni, A. (IT)
Bonasoni, P. (IT)
Duchi, R. (IT)Source Title Atmospheric Chemistry and Physics. - : Copernicus - ISSN 1680-7316
Roč. 11, č. 23 (2011), s. 12007-12036Number of pages 30 s. Language eng - English Country DE - Germany Keywords primary aerosol ; secondary aerosol ; boundary layer Subject RIV CF - Physical ; Theoretical Chemistry CEZ AV0Z40720504 - UCHP-M (2005-2011) UT WOS 000298134300006 EID SCOPUS 83455231344 DOI 10.5194/acp-11-12007-2011 Annotation It is important to understand the relative contribution of primary and secondary particles to regional and global aerosol so that models can attribute aerosol radiative forcing to different sources. In large-scale models, there is considerable uncertainty associated with treatments of particle formation (nucleation) in the boundary layer (BL) and in the size distribution of emitted primary particles, leading to uncertainties in predicted cloud condensation nuclei (CCN) concentrations. Here we quantify how primary particle emissions and secondary particle formation influence size-resolved particle number concentrations in the BL using a global aerosol microphysics model and aircraft and ground site observations made during the May 2008 campaign of the EUCAARI. We tested four different parameterisations for BL nucleation and two assumptions for the emission size distribution of anthropogenic and wildfire carbonaceous particles. Workplace Institute of Chemical Process Fundamentals Contact Eva Jirsová, jirsova@icpf.cas.cz, Tel.: 220 390 227 Year of Publishing 2012
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