Articles | Volume 18, issue 14
Atmos. Chem. Phys., 18, 10759–10772, 2018
https://doi.org/10.5194/acp-18-10759-2018
Atmos. Chem. Phys., 18, 10759–10772, 2018
https://doi.org/10.5194/acp-18-10759-2018

Research article 27 Jul 2018

Research article | 27 Jul 2018

Simulation of atmospheric organic aerosol using its volatility–oxygen-content distribution during the PEGASOS 2012 campaign

Eleni Karnezi et al.

Download

Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version Supplement - Supplement

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Spyros Pandis on behalf of the Authors (12 Jun 2018)  Author's response
ED: Referee Nomination & Report Request started (19 Jun 2018) by Thomas Röckmann
RR by Anonymous Referee #1 (02 Jul 2018)
ED: Publish as is (02 Jul 2018) by Thomas Röckmann
Download
Short summary
Different parameterizations of the organic aerosol (OA) formation and evolution are evaluated using ground and airborne measurements collected in the 2012 PEGASOS field campaign in the Po Valley (Italy). Total OA concentration and O : C ratios were reproduced within experimental error by a number of schemes. Anthropogenic secondary OA (SOA) contributed 15–25 % of the total OA, 20–35 % of SOA from intermediate volatility compounds oxidation, and 15–45 % of biogenic SOA depending on the scheme.
Altmetrics
Final-revised paper
Preprint