Open AccessRapid aerosol particle growth and increase of cloud condensation nucleus activity by secondary aerosol formation and condensation: A case study for regional air pollution in northeastern China
Author(s) -
Wiedensohler A.,
Cheng Y. F.,
Nowak A.,
Wehner B.,
Achtert P.,
Berghof M.,
Birmili W.,
Wu Z. J.,
Hu M.,
Zhu T.,
Takegawa N.,
Kita K.,
Kondo Y.,
Lou S. R.,
Hofzumahaus A.,
Holland F.,
Wahner A.,
Gunthe S. S.,
Rose D.,
Su H.,
Pöschl U.
Publication year - 2009
Publication title -
journal of geophysical research: atmospheres
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.67
H-Index - 298
eISSN - 2156-2202
pISSN - 0148-0227
DOI - 10.1029/2008jd010884
Subject(s) - aerosol , cloud condensation nuclei , nucleation , particle number , particle (ecology) , environmental science , mass concentration (chemistry) , atmospheric sciences , sulfate , condensation , chemistry , meteorology , physics , geology , thermodynamics , oceanography , organic chemistry , volume (thermodynamics)
This study was part of the international field measurement Campaigns of Air Quality Research in Beijing and Surrounding Region 2006 (CAREBeijing‐2006). We investigated a new particle formation event in a highly polluted air mass at a regional site south of the megacity Beijing and its impact on the abundance and properties of cloud condensation nuclei (CCN). During the 1‐month observation, particle nucleation followed by significant particle growth on a regional scale was observed frequently (∼30%), and we chose 23 August 2006 as a representative case study. Secondary aerosol mass was produced continuously, with sulfate, ammonium, and organics as major components. The aerosol mass growth rate was on average 19 μ g m −3 h −1 during the late hours of the day. This growth rate was observed several times during the 1‐month intensive measurements. The nucleation mode grew very quickly into the size range of CCN, and the CCN size distribution was dominated by the growing nucleation mode (up to 80% of the total CCN number concentration) and not as usual by the accumulation mode. At water vapor supersaturations of 0.07–0.86%, the CCN number concentrations reached maximum values of 4000–19,000 cm −3 only 6–14 h after the nucleation event. During particle formation and growth, the effective hygroscopicity parameter κ increased from about 0.1–0.3 to 0.35–0.5 for particles with diameters of 40–90 nm, but it remained nearly constant at ∼0.45 for particles with diameters of ∼190 nm. This result is consistent with aerosol chemical composition data, showing a pronounced increase of sulfate.