Articles | Volume 23, issue 2
https://doi.org/10.5194/acp-23-1209-2023
https://doi.org/10.5194/acp-23-1209-2023
Research article
 | 
24 Jan 2023
Research article |  | 24 Jan 2023

Modeling daytime and nighttime secondary organic aerosol formation via multiphase reactions of biogenic hydrocarbons

Sanghee Han and Myoseon Jang

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Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on "Modeling Diurnal Variation of SOA Formation via Multiphase Reactions of Biogenic Hydrocarbons"', Anonymous Referee #1, 23 Aug 2022
    • AC1: 'Reply on RC1', Myoseon Jang, 28 Oct 2022
  • RC2: 'Comment on acp-2022-327', Anonymous Referee #2, 18 Sep 2022
    • AC2: 'Reply on RC2', Myoseon Jang, 28 Oct 2022

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Myoseon Jang on behalf of the Authors (28 Oct 2022)  Author's response    Author's tracked changes    Manuscript
ED: Referee Nomination & Report Request started (29 Oct 2022) by Thomas Berkemeier
RR by Anonymous Referee #1 (10 Nov 2022)
RR by Anonymous Referee #3 (11 Nov 2022)
ED: Reconsider after major revisions (14 Nov 2022) by Thomas Berkemeier
AR by Myoseon Jang on behalf of the Authors (18 Nov 2022)  Author's response    Author's tracked changes    Manuscript
ED: Referee Nomination & Report Request started (19 Nov 2022) by Thomas Berkemeier
ED: Publish subject to minor revisions (review by editor) (04 Dec 2022) by Thomas Berkemeier
AR by Myoseon Jang on behalf of the Authors (13 Dec 2022)  Author's response    Author's tracked changes    Manuscript
ED: Publish as is (13 Dec 2022) by Thomas Berkemeier
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Short summary
The diurnal pattern in biogenic secondary organic aerosol (SOA) formation is simulated by using the UNIPAR model, which predicts SOA growth via multiphase reactions of hydrocarbons under varying NOx levels, aerosol acidity, humidity, and temperature. The simulation suggests that nighttime SOA formation, even in urban environments, where anthropogenic emission is high, is dominated by products from ozonolysis and NO3-initiated oxidation of biogenic hydrocarbons.
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