Positive trends in Southern Hemisphere carbonyl sulfide

Transport of carbonyl sulfide (OCS) from the troposphere to the stratosphere contributes sulfur to the stratospheric aerosol layer, which reflects incoming short‐wave solar radiation, cooling the climate system. Previous analyses of OCS observations have shown no significant trend, suggesting that O...

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Published inGeophysical research letters Vol. 42; no. 21; pp. 9473 - 9480
Main Authors Kremser, Stefanie, Jones, Nicholas B., Palm, Mathias, Lejeune, Bernard, Wang, Yuting, Smale, Dan, Deutscher, Nicholas M.
Format Journal Article Web Resource
LanguageEnglish
Published Washington Blackwell Publishing Ltd 16.11.2015
John Wiley & Sons, Inc
American Geophysical Union
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Summary:Transport of carbonyl sulfide (OCS) from the troposphere to the stratosphere contributes sulfur to the stratospheric aerosol layer, which reflects incoming short‐wave solar radiation, cooling the climate system. Previous analyses of OCS observations have shown no significant trend, suggesting that OCS is unlikely to be a major contributor to the reported increases in stratospheric aerosol loading and indicating a balanced OCS budget. Here we present analyses of ground‐based Fourier transform spectrometer measurements of OCS at three Southern Hemisphere sites spanning 34.45°S to 77.80°S. At all three sites statistically significant positive trends are seen from 2001 to 2014 with an observed overall trend in total column OCS at Wollongong of 0.73 ± 0.03%/yr, at Lauder of 0.43 ± 0.02%/yr, and at Arrival Heights of 0.45 ± 0.05%/yr. These observed trends in OCS imply that the OCS budget is not balanced and could contribute to constraints on current estimates of sources and sinks. Key Points First observed positive trend in OCS in the Southern Hemisphere Observed trends indicate imbalanced OCS budget Temporal structure of trend is similar across middle‐ and high‐latitude sites
Bibliography:ark:/67375/WNG-CHZ683ST-2
ArticleID:GRL53642
Australian Research Council - No. DP110101948; No. LE0668470
Marsden Fast-Start Fund
EU project StratoClim
Deutsche Forschungsgemeinschaft, DFG - No. PA 1714/6-1
istex:4ABABD0F1706B3709477E759433DFFE088D5712D
ObjectType-Article-1
SourceType-Scholarly Journals-1
ObjectType-Feature-2
content type line 23
scopus-id:2-s2.0-84954558994
ISSN:0094-8276
1944-8007
1944-8007
DOI:10.1002/2015GL065879