Počet záznamů: 1  

Comparison of Atmospheric New Particle Formation Events Events in Three Central European Cities.

  1. 1.
    SYSNO ASEP0487756
    Druh ASEPJ - Článek v odborném periodiku
    Zařazení RIVJ - Článek v odborném periodiku
    Poddruh JČlánek ve WOS
    NázevComparison of Atmospheric New Particle Formation Events Events in Three Central European Cities.
    Tvůrce(i) Németh, Z. (HU)
    Rosati, B. (AT)
    Zíková, Naděžda (UCHP-M) RID, ORCID, SAI
    Salma, I. (HU)
    Bozó, L. (HU)
    Dameto de España, C. (AT)
    Schwarz, Jaroslav (UCHP-M) RID, ORCID, SAI
    Ždímal, Vladimír (UCHP-M) RID, ORCID, SAI
    Wonaschütz, A. (AT)
    Zdroj.dok.Atmospheric Environment. - : Elsevier - ISSN 1352-2310
    Roč. 178, APR 2018 (2018), s. 191-197
    Poč.str.7 s.
    Jazyk dok.eng - angličtina
    Země vyd.GB - Velká Británie
    Klíč. slovaurban environment ; ultrafine particles ; new particle formation
    Vědní obor RIVDG - Vědy o atmosféře, meteorologie
    Obor OECDMeteorology and atmospheric sciences
    CEPLM2015037 GA MŠMT - Ministerstvo školství, mládeže a tělovýchovy
    Institucionální podporaUCHP-M - RVO:67985858
    UT WOS000428104200021
    EID SCOPUS85041381486
    DOI10.1016/j.atmosenv.2018.01.035
    AnotaceSimultaneous particle number size distribution measurements were performed in the urban environment of Budapest, Vienna, and Prague, three Central European cities located within 450 km of each other. The measurement days from the continuous, 2-year long campaign were classified for new particle formation (NPF) events using an adapted classification scheme for urban sites. The total numbers of NPF event days were 152 for Budapest, 69 for Vienna, and 143 for Prague. There were 12 days when new particle formation took place at all three sites. 11 out of these 12 days were in spring and in summer. There were only 2 (Budapest-Vienna), 19 (Budapest-Prague), and 19 (Vienna-Prague) nucleation days, when NPF did not occur on the third site. The main difference was related to source and sink terms of gas-phase sulphuric acid. Air mass origin and back-trajectories did not show any substantial influence on the atmospheric nucleation phenomena. The relative contribution of particles from NPF with respect to regional aerosol to the particles originating from all sources was expressed as nucleation strength factor. The overall mean nucleation strength factors were 1.58, 1.54, and 2.01 for Budapest, Vienna, and Prague, respectively, and showed diurnal and seasonal variations. The monthly mean NSF varied from 1.2 to 3.2 in Budapest, from 0.7 to 1.9 in Vienna, and from 1.0 to 2.3 in Prague. This implies that the new particle formation in cities is a significant source of ultrafine (UF) particles, and the amount of them is comparable to the directly emitted UF particles.
    PracovištěÚstav chemických procesů
    KontaktEva Jirsová, jirsova@icpf.cas.cz, Tel.: 220 390 227
    Rok sběru2019
Počet záznamů: 1  

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