Articles | Volume 18, issue 3
https://doi.org/10.5194/acp-18-1923-2018
https://doi.org/10.5194/acp-18-1923-2018
Research article
 | 
12 Feb 2018
Research article |  | 12 Feb 2018

Atmospheric carbonyl sulfide (OCS) measured remotely by FTIR solar absorption spectrometry

Geoffrey C. Toon, Jean-Francois L. Blavier, and Keeyoon Sung

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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 Geoff Toon on behalf of the Authors (14 Nov 2017)  Author's response   Manuscript 
ED: Publish as is (21 Nov 2017) by Hal Maring
AR by Geoff Toon on behalf of the Authors (20 Dec 2017)
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Short summary
OCS is the main form of atmospheric sulfur. It is produced near the earth's surface and destroyed primarily in the stratosphere, where it is converted to stratospheric sulfate aerosol (SSA). SSA plays an important role in atmospheric chemistry and transport and so it is important to better understand the factors that regulate OCS and hence SSA. Ground-based and balloon-borne infrared spectra observed over the past 30 years are analyzed to provide an improved OCS dataset.
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