Regular Article
Identification of marine and continental aerosol sources in Paris using high resolution aerosol mass spectrometry
Article first published online: 19 FEB 2013
DOI: 10.1002/jgrd.50151
©2013. American Geophysical Union. All Rights Reserved.
Issue

Journal of Geophysical Research: Atmospheres
Volume 118, Issue 4, pages 1950–1963, 27 February 2013
Additional Information
How to Cite
, et al. (2013), Identification of marine and continental aerosol sources in Paris using high resolution aerosol mass spectrometry, J. Geophys. Res. Atmos., 118, 1950–1963, doi:10.1002/jgrd.50151.
Publication History
- Issue published online: 17 APR 2013
- Article first published online: 19 FEB 2013
- Manuscript Accepted: 25 NOV 2012
- Manuscript Revised: 5 NOV 2012
- Manuscript Received: 20 AUG 2012
Keywords:
- aerosol mass spectrometry;
- source apportionment;
- urban aerosol;
- marine aerosol
[1] Major summertime aerosol emission sources in Paris were assessed using a high resolution time-of-flight aerosol mass spectrometer (HR-ToF-AMS). The application of positive matrix factorization (PMF) to the highly mass and time-resolved AMS measurements allowed the identification of primary and secondary sources of organic (OA) and sulfate aerosols. Primary anthropogenic emissions contributed on average ~27% (14.7% cooking, 12% traffic) to the total organic mass, while the major contribution to the organic fraction was associated with secondary formation products. Low-volatility oxygenated OA (LV-OOA, 25.2%) and semi-volatile oxygenated OA (SV-OOA, 32.4%) factors were classified as SOA. An additional component with high S : C and O : C ratios was identified and attributed to marine emissions (marine organic aerosol, MOA), owing to its high correlation with methanesulfonic acid (R2 = 0.84) and contributing on average 15.7% to the total OA mass, even in the continental megacity of Paris. Non-sea salt sulfate was apportioned by including both organic and sulfate ions in the PMF data matrix. This allowed apportionment of submicron sulfate to continental versus marine sources. A detailed source apportionment of PM1 combining AMS, aethalometer, and filter data is presented.

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