Articles | Volume 18, issue 18
https://doi.org/10.5194/acp-18-13617-2018
https://doi.org/10.5194/acp-18-13617-2018
Research article
 | 
27 Sep 2018
Research article |  | 27 Sep 2018

DMS oxidation and sulfur aerosol formation in the marine troposphere: a focus on reactive halogen and multiphase chemistry

Qianjie Chen, Tomás Sherwen, Mathew Evans, and Becky Alexander

Viewed

Total article views: 6,146 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
3,966 2,107 73 6,146 96 165
  • HTML: 3,966
  • PDF: 2,107
  • XML: 73
  • Total: 6,146
  • BibTeX: 96
  • EndNote: 165
Views and downloads (calculated since 02 May 2018)
Cumulative views and downloads (calculated since 02 May 2018)

Viewed (geographical distribution)

Total article views: 6,146 (including HTML, PDF, and XML) Thereof 6,182 with geography defined and -36 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Discussed (final revised paper)

Latest update: 23 Nov 2024
Download
Short summary
Uncertainty in the natural tropospheric sulfur cycle represents the largest source of uncertainty in radiative forcing estimates of sulfate aerosol. This study investigates the natural sulfur cycle in the marine troposphere using the GEOS-Chem model. We found that BrO is important for DMS oxidation and multiphase chemistry is important for MSA production and loss, which have implications for the yield of SO2 and MSA from DMS oxidation and the radiative effect of DMS-derived sulfate aerosol.
Altmetrics
Final-revised paper
Preprint