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ACP | Articles | Volume 19, issue 23
Atmos. Chem. Phys., 19, 14455–14476, 2019
https://doi.org/10.5194/acp-19-14455-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.

Special issue: NETCARE (Network on Aerosols and Climate: Addressing Key Uncertainties...

Atmos. Chem. Phys., 19, 14455–14476, 2019
https://doi.org/10.5194/acp-19-14455-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.

Research article 29 Nov 2019

Research article | 29 Nov 2019

Dimethyl sulfide and its role in aerosol formation and growth in the Arctic summer – a modelling study

Roghayeh Ghahremaninezhad et al.

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AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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AR: Author's response | RR: Referee report | ED: Editor decision
AR by Roya Ghahreman on behalf of the Authors (11 Sep 2019)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (12 Sep 2019) by Lynn M. Russell
RR by Anonymous Referee #2 (25 Sep 2019)
RR by Anonymous Referee #4 (25 Oct 2019)
ED: Publish subject to minor revisions (review by editor) (28 Oct 2019) by Lynn M. Russell
AR by Roya Ghahreman on behalf of the Authors (28 Oct 2019)  Author's response    Manuscript
ED: Publish as is (30 Oct 2019) by Lynn M. Russell
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Short summary
Atmospheric DMS(g) is a climatically important compound and the main source of biogenic sulfate in the Arctic. Its abundance in the Arctic increases during summer due to greater ice-free sea surface and higher biological activity. In this study, we implemented DMS(g) in a regional air quality forecast model configured for the Arctic. The study showed a significant impact from DMS(g) on sulfate aerosols, particularly in the 50–100 nm size range, in the Arctic marine boundary layer during summer.
Atmospheric DMS(g) is a climatically important compound and the main source of biogenic sulfate...
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