Biogenic emissions and land–atmosphere interactions as drivers of the daytime evolution of secondary organic aerosol in the southeastern US

Nagori, Juhi; Janssen, Ruud H. H.; Fry, Juliane L.; Krol, Maarten; Jimenez, Jose L.; Hu, Weiwei; Vilà-Guerau de Arellano, Jordi

doi:https://doi.org/10.5194/acp-19-701-2019

Articles | Volume 19, issue 2

https://doi.org/10.5194/acp-19-701-2019

© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.

https://doi.org/10.5194/acp-19-701-2019

© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.

Articles | Volume 19, issue 2

Research article

|

18 Jan 2019

Research article |

| 18 Jan 2019

Biogenic emissions and land–atmosphere interactions as drivers of the daytime evolution of secondary organic aerosol in the southeastern US

Juhi Nagori, Ruud H. H. Janssen, Juliane L. Fry, Maarten Krol, Jose L. Jimenez, Weiwei Hu, and Jordi Vilà-Guerau de Arellano

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Final revised paper (published on 18 Jan 2019)
Preprint (discussion started on 10 Aug 2018)

Interactive discussion

Status: closed

AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment

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RC1: 'review comments', Anonymous Referee #1, 06 Sep 2018
RC2: 'Reviewer #2', Anonymous Referee #2, 18 Sep 2018
AC1: 'Author comments', Juhi Nagori, 09 Nov 2018

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision

AR by Juhi Nagori on behalf of the Authors (23 Nov 2018) Author's response Manuscript

ED: Referee Nomination & Report Request started (26 Nov 2018) by Manabu Shiraiwa

RR by Anonymous Referee #1 (03 Dec 2018)

ED: Publish as is (03 Dec 2018) by Manabu Shiraiwa

AR by Juhi Nagori on behalf of the Authors (11 Dec 2018) Author's response Manuscript

Short summary

Secondary organic aerosol (SOA) is produced through a complex interaction of sunlight, volatile organic compounds emitted from trees, anthropogenic emissions, and atmospheric chemistry. We are able to successfully model the formation and diurnal evolution of SOA using a model that takes into consideration the surface and boundary layer dynamics (1–2 km from the surface) and photochemistry above the southeastern US with data collected during the SOAS campaign to constrain the model.