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The strength of the meridional overturning circulation of the stratosphere.

Accepted version
Peer-reviewed

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Article

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Authors

Linz, Marianna 
Plumb, R Alan 
Gerber, Edwin P 
Haenel, Florian J 
Stiller, Gabriele 

Abstract

The distribution of gases such as ozone and water vapour in the stratosphere - which affect surface climate - is influenced by the meridional overturning of mass in the stratosphere, the Brewer-Dobson circulation. However, observation-based estimates of its global strength are difficult to obtain. Here we present two calculations of the mean strength of the meridional overturning of the stratosphere. We analyze satellite data that document the global diabatic circulation between 2007- 2011, and compare these to three re-analysis data sets and to simulations with a state-of-the-art chemistry-climate model. Using measurements of sulfur hexafluoride (SF6) and nitrous oxide, we calculate the global mean diabatic overturning mass flux throughout the stratosphere. In the lower stratosphere, these two estimates agree, and at a potential temperature level of 460 K (about 20 km or 60 hPa in tropics), the global circulation strength is 6.3-7.6 × 109 kg/s. Higher in the atmosphere, only the SF6-based estimate is available, and it diverges from the re-analysis data and simulations. Interpretation of the SF6 data-based estimate is limited because of a mesospheric sink of SF6; however, the reanalyses also differ substantially from each other. We conclude that the uncertainty in the mean meridional overturning circulation strength at upper levels of the stratosphere amounts to at least 100 %.

Description

Keywords

0401 Atmospheric Sciences

Journal Title

Nat Geosci

Conference Name

Journal ISSN

1752-0894
1752-0908

Volume Title

10

Publisher

Springer Science and Business Media LLC

Rights

All rights reserved
Sponsorship
European Research Council (267760)