References

ACP

Atmospheric Chemistry and Physics

ACP

1680-7324

Copernicus GmbH

Göttingen, Germany

10.5194/acp-12-3147-2012

Nucleation and condensational growth to CCN sizes during a sustained pristine biogenic SOA event in a forested mountain valley

Pierce

J. R.

¹ Leaitch

W. R.

² Liggio

² Westervelt

D. M.

³ Wainwright

C. D.

¹ Abbatt

J. P. D.

⁴ Ahlm

⁵ Al-Basheer

² Cziczo

D. J.

⁶ Hayden

K. L.

² Lee

A. K. Y.

⁴ Li

S.-M.

² Russell

L. M.

⁵ Sjostedt

S. J.

² Strawbridge

K. B.

² Travis

² Vlasenko

² Wentzell

J. J. B.

² Wiebe

H. A.

² Wong

J. P. S.

⁴ Macdonald

A. M.

Department of Physics and Atmospheric Science, Dalhousie University, Halifax, Nova Scotia, Canada

Environment Canada, Toronto, Ontario, Canada

Department of Civil and Environment Engineering, Carnegie Mellon University, Pittsburgh, PA, USA

Department of Chemistry, University of Toronto, Toronto, Ontario, Canada

Scripps Institution of Oceanography, University of California-San Diego, La Jolla, CA, USA

Department of Earth, Atmospheric and Planetary Sciences, Massachusetts Institute of Technology, Boston, MA, USA

02 04 2012

12 7 3147 3163

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The Whistler Aerosol and Cloud Study (WACS 2010), included intensive measurements of trace gases and particles at two sites on Whistler Mountain. Between 6–11 July 2010 there was a sustained high-pressure system over the region with cloud-free conditions and the highest temperatures of the study. During this period, the organic aerosol concentrations rose from <1 μg m−3 to &sim;6 μg m−3. Precursor gas and aerosol composition measurements show that these organics were almost entirely of secondary biogenic nature. Throughout 6–11 July, the anthropogenic influence was minimal with sulfate concentrations <0.2 μg m−3 and SO2 mixing ratios ≈ 0.05–0.1 ppbv. Thus, this case provides excellent conditions to probe the role of biogenic secondary organic aerosol in aerosol microphysics. Although SO2 mixing ratios were relatively low, box-model simulations show that nucleation and growth may be modeled accurately if Jnuc = 3 × 10−7[H2SO4] and the organics are treated as effectively non-volatile. Due to the low condensation sink and the fast condensation rate of organics, the nucleated particles grew rapidly (2–5 nm h−1) with a 10–25% probability of growing to CCN sizes (100 nm) in the first two days as opposed to being scavenged by coagulation with larger particles. The nucleated particles were observed to grow to &sim;200 nm after three days. Comparisons of size-distribution with CCN data show that particle hygroscopicity (κ) was &sim;0.1 for particles larger 150 nm, but for smaller particles near 100 nm the κ value decreased near midway through the period from 0.17 to less than 0.06. In this environment of little anthropogenic influence and low SO2, the rapid growth rates of the regionally nucleated particles – due to condensation of biogenic SOA – results in an unusually high efficiency of conversion of the nucleated particles to CCN. Consequently, despite the low SO2, nucleation/growth appear to be the dominant source of particle number.

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