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Primary Versus Secondary Contributions to Particle Number Concentrations in the European Boundary Layer

  1. 1.
    SYSNO ASEP0372230
    Document TypeJ - Journal Article
    R&D Document TypeJournal Article
    Subsidiary JČlánek ve WOS
    TitlePrimary 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 TitleAtmospheric Chemistry and Physics. - : Copernicus - ISSN 1680-7316
    Roč. 11, č. 23 (2011), s. 12007-12036
    Number of pages30 s.
    Languageeng - English
    CountryDE - Germany
    Keywordsprimary aerosol ; secondary aerosol ; boundary layer
    Subject RIVCF - Physical ; Theoretical Chemistry
    CEZAV0Z40720504 - UCHP-M (2005-2011)
    UT WOS000298134300006
    EID SCOPUS83455231344
    DOI10.5194/acp-11-12007-2011
    AnnotationIt 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.
    WorkplaceInstitute of Chemical Process Fundamentals
    ContactEva Jirsová, jirsova@icpf.cas.cz, Tel.: 220 390 227
    Year of Publishing2012
Number of the records: 1  

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