CCN predictions using simplified assumptions of organic aerosol composition and mixing state: a synthesis from six different locations

被引:100
作者
Ervens, B. [1 ,2 ]
Cubison, M. J. [1 ]
Andrews, E. [1 ,2 ]
Feingold, G. [2 ]
Ogren, J. A. [2 ]
Jimenez, J. L. [1 ,3 ]
Quinn, P. K. [4 ]
Bates, T. S. [4 ]
Wang, J. [5 ]
Zhang, Q. [6 ]
Coe, H.
Flynn, M.
Allan, J. D. [7 ]
机构
[1] Univ Colorado, CIRES, Boulder, CO 80309 USA
[2] NOAA, Earth Syst Res Lab, Boulder, CO USA
[3] Univ Colorado, Dept Chem & Biochem, Boulder, CO 80309 USA
[4] NOAA, Pacific Marine Environm Lab, Seattle, WA 98115 USA
[5] Brookhaven Natl Lab, Upton, NY 11973 USA
[6] Univ Calif Davis, Dept Environm Toxicol, Davis, CA 95616 USA
[7] Univ Manchester, Sch Earth Atmospher & Environm Sci, Natl Ctr Atmospher Sci, Manchester M13 9PL, Lancs, England
关键词
CLOUD CONDENSATION NUCLEI; SIZE-RESOLVED MEASUREMENTS; HYGROSCOPIC PROPERTIES; CHEMICAL-COMPOSITION; GROWTH; CHEMISTRY; CLOSURE; ACTIVATION; MARINE; CITY;
D O I
10.5194/acp-10-4795-2010
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
An accurate but simple quantification of the fraction of aerosol particles that can act as cloud condensation nuclei (CCN) is needed for implementation in large-scale models. Data on aerosol size distribution, chemical composition, and CCN concentration from six different locations have been analyzed to explore the extent to which simple assumptions of composition and mixing state of the organic fraction can reproduce measured CCN number concentrations. Fresher pollution aerosol as encountered in Riverside, CA, and the ship channel in Houston, TX, cannot be represented without knowledge of more complex (size-resolved) composition. For aerosol that has experienced processing (Mexico City, Holme Moss (UK), Point Reyes (CA), and Chebogue Point (Canada)), CCN can be predicted within a factor of two assuming either externally or internally mixed soluble organics although these simplified compositions/mixing states might not represent the actual properties of ambient aerosol populations, in agreement with many previous CCN studies in the literature. Under typical conditions, a factor of two uncertainty in CCN concentration due to composition assumptions translates to an uncertainty of similar to 15% in cloud drop concentration, which might be adequate for large-scale models given the much larger uncertainty in cloudiness.
引用
收藏
页码:4795 / 4807
页数:13
相关论文
共 54 条
[1]   Organic aerosol formation in urban and industrial plumes near Houston and Dallas, Texas [J].
Bahreini, R. ;
Ervens, B. ;
Middlebrook, A. M. ;
Warneke, C. ;
de Gouw, J. A. ;
DeCarlo, P. F. ;
Jimenez, J. L. ;
Brock, C. A. ;
Neuman, J. A. ;
Ryerson, T. B. ;
Stark, H. ;
Atlas, E. ;
Brioude, J. ;
Fried, A. ;
Holloway, J. S. ;
Peischl, J. ;
Richter, D. ;
Walega, J. ;
Weibring, P. ;
Wollny, A. G. ;
Fehsenfeld, F. C. .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2009, 114
[2]   Boundary layer aerosol chemistry during TexAQS/GoMACCS 2006: Insights into aerosol sources and transformation processes [J].
Bates, T. S. ;
Quinn, P. K. ;
Coffman, D. ;
Schulz, K. ;
Covert, D. S. ;
Johnson, J. E. ;
Williams, E. J. ;
Lerner, B. M. ;
Angevine, W. M. ;
Tucker, S. C. ;
Brewer, W. A. ;
Stohl, A. .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2008, 113
[3]   CCN activation of slightly soluble organics: the importance of small amounts of inorganic salt and particle phase [J].
Bilde, M ;
Svenningsson, B .
TELLUS SERIES B-CHEMICAL AND PHYSICAL METEOROLOGY, 2004, 56 (02) :128-134
[4]   Cloud condensation nuclei measurements in the marine boundary layer of the eastern Mediterranean: CCN closure and droplet growth kinetics [J].
Bougiatioti, A. ;
Fountoukis, C. ;
Kalivitis, N. ;
Pandis, S. N. ;
Nenes, A. ;
Mihalopoulos, N. .
ATMOSPHERIC CHEMISTRY AND PHYSICS, 2009, 9 (18) :7053-7066
[5]   Closure between measured and modeled cloud condensation nuclei (CCN) using size-resolved aerosol compositions in downtown Toronto [J].
Broekhuizen, K. ;
Chang, R. Y. -W. ;
Leaitch, W. R. ;
Li, S. -M. ;
Abbatt, J. P. D. .
ATMOSPHERIC CHEMISTRY AND PHYSICS, 2006, 6 :2513-2524
[6]   Chemical and microphysical characterization of ambient aerosols with the aerodyne aerosol mass spectrometer [J].
Canagaratna, M. R. ;
Jayne, J. T. ;
Jimenez, J. L. ;
Allan, J. D. ;
Alfarra, M. R. ;
Zhang, Q. ;
Onasch, T. B. ;
Drewnick, F. ;
Coe, H. ;
Middlebrook, A. ;
Delia, A. ;
Williams, L. R. ;
Trimborn, A. M. ;
Northway, M. J. ;
DeCarlo, P. F. ;
Kolb, C. E. ;
Davidovits, P. ;
Worsnop, D. R. .
MASS SPECTROMETRY REVIEWS, 2007, 26 (02) :185-222
[7]  
Chang R.Y.-W., 2009, Atmospheric Chemistry and Physics Discussions, V9, P25323, DOI [DOI 10.5194/ACPD-9-25323-2009, 10.5194/acpd-9-25323-2009]
[8]   CCN measurements during ACE-2 and their relationship to cloud microphysical properties [J].
Chuang, PY ;
Collins, DR ;
Pawlowska, H ;
Snider, JR ;
Jonsson, HH ;
Brenguier, JL ;
Flagan, RC ;
Seinfeld, JH .
TELLUS SERIES B-CHEMICAL AND PHYSICAL METEOROLOGY, 2000, 52 (02) :843-867
[9]  
Cocker DR, 2001, AEROSOL SCI TECH, V35, P637, DOI 10.1080/027868201316899992
[10]   Aerosol-cloud drop concentration closure in warm cumulus [J].
Conant, WC ;
VanReken, TM ;
Rissman, TA ;
Varutbangkul, V ;
Jonsson, HH ;
Nenes, A ;
Jimenez, JL ;
Delia, AE ;
Bahreini, R ;
Roberts, GC ;
Flagan, RC ;
Seinfeld, JH .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2004, 109 (D13) :D132041-12