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Organic aerosol composition and sources in Pasadena, California, during the 2010 CalNex campaign

  • 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, J. L. Jimenez*
*Corresponding author for this work
  • Cooperative Institute for Research in Environmental Sciences
  • University of Colorado Boulder
  • National Oceanic and Atmospheric Administration
  • University of California at Davis
  • Peking University
  • University of Houston
  • University of Manchester
  • Aerodyne Research, Inc.
  • Georgia Institute of Technology
  • University of California at San Diego
  • University of California at Berkeley
  • Aerosol Dynamics Inc.
  • University of North Carolina at Chapel Hill
  • United States Environmental Protection Agency
  • Indiana University Bloomington
  • Université de Lille
  • IMT Nord Europe

Research output: Contribution to journalArticlepeer-review

Abstract

Organic aerosols (OA) in Pasadena are characterized using multiple measurements from the California Research at the Nexus of Air Quality and Climate Change (CalNex) campaign. Five OA components are identified using positive matrix factorization including hydrocarbon-like OA (HOA) and two types of oxygenated OA (OOA). The Pasadena OA elemental composition when plotted as H:C versus O:C follows a line less steep than that observed for Riverside, CA. The OOA components from both locations follow a common line, however, indicating similar secondary organic aerosol (SOA) oxidation chemistry at the two sites such as fragmentation reactions leading to acid formation. In addition to the similar evolution of elemental composition, the dependence of SOA concentration on photochemical age displays quantitatively the same trends across several North American urban sites. First, the OA/ΔCO values for Pasadena increase with photochemical age exhibiting a slope identical to or slightly higher than those for Mexico City and the northeastern United States. Second, the ratios of OOA to odd-oxygen (a photochemical oxidation marker) for Pasadena, Mexico City, and Riverside are similar, suggesting a proportional relationship between SOA and odd-oxygen formation rates. Weekly cycles of the OA components are examined as well. HOA exhibits lower concentrations on Sundays versus weekdays, and the decrease in HOA matches that predicted for primary vehicle emissions using fuel sales data, traffic counts, and vehicle emission ratios. OOA does not display a weekly cycle - after accounting for differences in photochemical aging - which suggests the dominance of gasoline emissions in SOA formation under the assumption that most urban SOA precursors are from motor vehicles.

Original languageEnglish
Pages (from-to)9233-9257
Number of pages25
JournalJournal of Geophysical Research: Atmospheres
Volume118
Issue number16
DOIs
StatePublished - 27 Aug 2013
Externally publishedYes

UN SDGs

This output contributes to the following UN Sustainable Development Goals (SDGs)

  1. SDG 11 - Sustainable Cities and Communities
    SDG 11 Sustainable Cities and Communities
  2. SDG 13 - Climate Action
    SDG 13 Climate Action

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