Modeling new particle formation during air pollution episodes: Impacts on aerosol and cloud condensation nuclei

被引:30
作者
Sotiropoulou, R. E. P.
Tagaris, E.
Pilinis, C.
Anttila, T.
Kulmala, M.
机构
[1] Univ Aegean, Dept Environm, Mitilini 81100, Lesvos, Greece
[2] Georgia Inst Technol, Dept Earth & Atmospher Sci, Atlanta, GA 30332 USA
[3] Georgia Inst Technol, Dept Civil & Environm Engn, Atlanta, GA 30332 USA
[4] Finnish Meteorol Inst, FIN-00101 Helsinki, Finland
[5] Forschungszentrum Julich, ICG Troposphare 2, Julich, Germany
[6] Univ Helsinki, Dept Phys Sci, Helsinki, Finland
关键词
D O I
10.1080/02786820600714346
中图分类号
TQ [化学工业];
学科分类号
0817 ;
摘要
The impact of new particle formation on regional air quality and CCN formation is for the first time explored using the UAM-AERO air quality model. New particles are formed by ternary nucleation of sulfuric acid, ammonia and water; subsequent growth of clusters to large sizes is driven by condensation of sulfuric acid and organic vapors, as described by the recently developed nano-Kohler theory. Application of the model in Athens (GAA) and Marseilles (GMA) reveals higher sulfuric acid condensational sink and gaseous sulfuric acid (hence nucleation rate) for the latter. However, limited quantities of organic vapors in the GMA inhibit the growth of the formed clusters; therefore new particle formation is more efficient in the GAA. A sensitivity analysis demonstrates that (1) uncertainty in vaporization enthalpy does not affect organic carbon formed by nucleation, and (2) an accommodation coefficient of unity gives excellent agreement of condensation sink with in-situ observations. Nucleation affects the aerosol size distribution, and can be an important contributor to CCN; locally it can be more important than chemical ageing of pre-existing aerosols.
引用
收藏
页码:557 / 572
页数:16
相关论文
共 78 条
[1]   ADREA-I - A 3-DIMENSIONAL TRANSIENT TRANSPORT CODE FOR COMPLEX TERRAIN AND OTHER APPLICATIONS [J].
BARTZIS, JG ;
VENETSANOS, AG ;
VARVAYANNI, M ;
CATSAROS, N ;
MEGARITOU, A .
NUCLEAR TECHNOLOGY, 1991, 94 (02) :135-148
[2]  
BARTZIS JG, 2004, EUR AER C EAC 2004 B
[3]  
BREINBJER B, 2003, EUR AER C MADR SEPT
[4]   Categorization of cold period weather types in Greece on the basis of the photointerpretation of NOAA/AVHRR imagery [J].
Cartalis, C ;
Chrysoulakis, N ;
Feidas, H ;
Pitsitakis, N .
INTERNATIONAL JOURNAL OF REMOTE SENSING, 2004, 25 (15) :2951-2977
[5]   A DETAILED MECHANISM FOR THE GAS-PHASE ATMOSPHERIC REACTIONS OF ORGANIC-COMPOUNDS [J].
CARTER, WPL .
ATMOSPHERIC ENVIRONMENT PART A-GENERAL TOPICS, 1990, 24 (03) :481-518
[6]   OCEANIC PHYTOPLANKTON, ATMOSPHERIC SULFUR, CLOUD ALBEDO AND CLIMATE [J].
CHARLSON, RJ ;
LOVELOCK, JE ;
ANDREAE, MO ;
WARREN, SG .
NATURE, 1987, 326 (6114) :655-661
[7]   Cloud condensation nucleus activity of organic compounds: a laboratory study [J].
Corrigan, CE ;
Novakov, T .
ATMOSPHERIC ENVIRONMENT, 1999, 33 (17) :2661-2668
[8]   A study of the ability of pure secondary organic aerosol to act as cloud condensation nuclei [J].
Cruz, CN ;
Pandis, SN .
ATMOSPHERIC ENVIRONMENT, 1997, 31 (15) :2205-2214
[9]   Chemical features and seasonal variation of fine aerosol water-soluble organic compounds in the Po Valley, Italy [J].
Decesari, S ;
Facchini, MC ;
Matta, E ;
Lettini, F ;
Mircea, M ;
Fuzzi, S ;
Tagliavini, E ;
Putaud, JP .
ATMOSPHERIC ENVIRONMENT, 2001, 35 (21) :3691-3699
[10]  
*ENVIRON INT CORP, 2004, US GUID COMPR AIR QU