Atmospheric Chemistry and Physics
Atmospheric Chemistry and Physics
ACP
Articles | Volume 23, issue 18
Articles | Volume 23, issue 18
https://doi.org/10.5194/acp-23-10609-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/acp-23-10609-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
Articles | Volume 23, issue 18
Measurement report
 | 
26 Sep 2023
Measurement report |  | 26 Sep 2023

Measurement report: Carbonyl sulfide production during dimethyl sulfide oxidation in the atmospheric simulation chamber SAPHIR

Marc von Hobe, Domenico Taraborrelli, Sascha Alber, Birger Bohn, Hans-Peter Dorn, Hendrik Fuchs, Yun Li, Chenxi Qiu, Franz Rohrer, Roberto Sommariva, Fred Stroh, Zhaofeng Tan, Sergej Wedel, and Anna Novelli

Viewed

Total article views: 1,628 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,173 408 47 1,628 100 36 77
  • HTML: 1,173
  • PDF: 408
  • XML: 47
  • Total: 1,628
  • Supplement: 100
  • BibTeX: 36
  • EndNote: 77
Views and downloads (calculated since 26 Apr 2023)
Cumulative views and downloads (calculated since 26 Apr 2023)

Viewed (geographical distribution)

Total article views: 1,628 (including HTML, PDF, and XML) Thereof 1,583 with geography defined and 45 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 30 Jan 2025
Download
Short summary
The trace gas carbonyl sulfide (OCS) transports sulfur from the troposphere to the stratosphere, where sulfate aerosols are formed that influence climate and stratospheric chemistry. An uncertain OCS source in the troposphere is chemical production form dimethyl sulfide (DMS), a gas released in large quantities from the oceans. We carried out experiments in a large atmospheric simulation chamber to further elucidate the chemical mechanism of OCS production from DMS.
Read more
Altmetrics
Final-revised paper
Preprint