Evidence for NO x Control over Nighttime SOA Formation

Author:

Rollins A. W.1,Browne E. C.1,Min K.-E.2,Pusede S. E.1,Wooldridge P. J.1,Gentner D. R.3,Goldstein A. H.34,Liu S.5,Day D. A.5,Russell L. M.5,Cohen R. C.12

Affiliation:

1. Department of Chemistry, University of California, Berkeley, Berkeley, CA 94720, USA.

2. Department of Earth and Planetary Sciences, University of California, Berkeley, Berkeley, CA 94720, USA.

3. Department of Civil and Environmetal Engineering, University of California, Berkeley, Berkeley, CA 94720, USA.

4. Department of Environmental Science, Policy, and Management, University of California, Berkeley, Berkeley, CA 94720, USA.

5. Scripps Institution of Oceanography, University of California, San Diego, San Diego, CA 92093, USA.

Abstract

Nighttime Sources Organic aerosols account for about half of the total mass of small (submicrometer) particles in the troposphere, and most of them are believed to form through the oxidation of volatile molecules, rather than being emitted directly from specific sources. These particles have important roles in many atmospheric processes, and therefore a better understanding of their complex composition and chemistry is desirable. Rollins et al. (p. 1210 ) report on measurements of particulate organic nitrates, an important class of organic aerosols that form at night. However, they also found that high concentrations of organic molecules can suppress the growth of organic nitrate particles. These observations should help improve efforts to reduce organic aerosol pollution.

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

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