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

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. Du...

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Veröffentlicht in:Atmospheric chemistry and physics 2012-04, Vol.12 (7), p.3147-3163
Hauptverfasser: Pierce, J. R, Leaitch, W. R, Liggio, J, Westervelt, D. M, Wainwright, C. D, Abbatt, J. P. D, Ahlm, L, Al-Basheer, W, Cziczo, D. J, Hayden, K. L, Lee, A. K. Y, Li, S.-M, Russell, L. M, Sjostedt, S. J, Strawbridge, K. B, Travis, M, Vlasenko, A, Wentzell, J. J. B, Wiebe, H. A, Wong, J. P. S, Macdonald, A. M
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Sprache:eng
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Zusammenfassung: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
ISSN:1680-7324
1680-7316
1680-7324
DOI:10.5194/acp-12-3147-2012