Dependence between the photochemical age of light aromatic hydrocarbons and the carbon isotope ratios of atmospheric nitrophenols

Saccon, Marina; Kornilova, Anna; Huang, Lin; Rudolph, Jochen

doi:https://doi.org/10.5194/acp-19-5495-2019

Articles | Volume 19, issue 8

https://doi.org/10.5194/acp-19-5495-2019

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

https://doi.org/10.5194/acp-19-5495-2019

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

Articles | Volume 19, issue 8

Research article

|

26 Apr 2019

Research article |

| 26 Apr 2019

Dependence between the photochemical age of light aromatic hydrocarbons and the carbon isotope ratios of atmospheric nitrophenols

Marina Saccon, Anna Kornilova, Lin Huang, and Jochen Rudolph

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Final revised paper (published on 26 Apr 2019)
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Preprint (discussion started on 26 Feb 2018)
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Interactive discussion

Status: closed

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

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RC1: 'Review of Saccon et al.', Anonymous Referee #1, 04 May 2018
RC2: 'Review on: Dependence between the Photochemical Age of Light Aromatic Hydrocarbons and the Carbon Isotope Ratios of Atmospheric Nitrophenols- by Saccon et al.', Anonymous Referee #3, 29 Jun 2018
AC1: 'Reply to Comments', M. Saccon, 02 Nov 2018

Peer-review completion

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

AR by Anna Mirena Feist-Polner on behalf of the Authors (07 Jan 2019) Author's response

ED: Referee Nomination & Report Request started (24 Jan 2019) by Rupert Holzinger

ED: Publish as is (12 Feb 2019) by Rupert Holzinger

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Short summary

As compound are emitted into the atmosphere, they can undergo chemical reactions to produce secondary products. This paper investigates the relations of compounds' unique chemical characteristics to the processes that formed them from emissions in the atmosphere. A model is applied to help with this investigation. The complexity of the atmosphere, including mixing of air masses and variability in precursor reactivity, is taken into consideration, and results are presented.