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P. L. Hayes, A. M. Ortega, M. J. Cubison, K. D. Froyd, Y. Zhao, S. S. Cliff, W. W. Hu, D. W. Toohey, J. H. Flynn, B. L. Lefer, N. Grossberg, S. Alvarez, B. Rappenglück, J. W. Taylor, J. D. Allan, J. S. Holloway, J. B. Gilman, W. C. Kuster, J. A. de Gouw, P. Massoli, X. Zhang, J. Liu, R. J. Weber, A. L. Corrigan, L. M. Russell, G. Isaacman, D. R. Worton, N. M. Kreisberg, A. H. Goldstein, R. Thalman, E. M. Waxman, R. Volkamer, Y. H. Lin, J. D. Surratt, T. E. Kleindienst, J. H. Offenberg, S. Dusanter, S. Griffith, P. S. Stevens, J. Brioude, W. M. Angevine and J. L. Jimenez Organic aerosol composition and sources in Pasadena, California, during the 2010 CalNex campaign Journal of Geophysical Research: Atmospheres 118

Version of Record online: 29 AUG 2013 | DOI: 10.1002/jgrd.50530

Key Points

  • For the same photochemical ages, SOA to CO ratios do not display a weekly cycle
  • Organic aerosol is apportioned into five components using PMF
  • SOA formation/evolution is similar for several urban locations

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