Is the Brewer‐Dobson circulation increasing or moving upward?. Issue 4 (25th February 2016)

• Record Type: Journal Article
• Authors: Oberländer‐Hayn, Sophie; Gerber, Edwin P.; Abalichin, Janna; Akiyoshi, Hideharu; Kerschbaumer, Andreas; Kubin, Anne; Kunze, Markus; Langematz, Ulrike; Meul, Stefanie; Michou, Martine; Morgenstern, Olaf; Oman, Luke D.
• Is Part Of: Geophysical research letters. Volume 43:Issue 4(2016)
• Page Start: 1772
• Page End: 1779
• Publication Date: 2016-02-25
• Subjects: stratosphere -- Brewer‐Dobson circulation -- tropical upward mass flux -- tropopause -- upward shift -- climate change; Geophysics -- Periodicals; Planets -- Periodicals; Lunar geology -- Periodicals; 550
• DOI: 10.1002/2015GL067545
• Languages: English
• ISSNs: 0094-8276

Abstract

Abstract: The meridional circulation of the stratosphere, or Brewer‐Dobson circulation (BDC), is projected to accelerate with increasing greenhouse gas (GHG) concentrations. The acceleration is typically quantified by changes in the tropical upward mass flux ( F trop ) across a given pressure surface. Simultaneously, models project a lifting of the entire atmospheric circulation in response to GHGs; notably, the tropopause rises about a kilometer over this century. In this study, it is shown that most of the BDC trend is associated with the rise in the circulation. Using a chemistry‐climate model (CCM), F trop trends across 100 hPa are contrasted with those across the tropopause: while F trop at 100 hPa increases 1–2 %/decade, the mass flux entering the atmosphere above the tropopause actually decreases. Similar results are found for other CCMs, suggesting that changes in the BDC may better be described as an upward shift of the circulation, as opposed to an increase, with implications for the mechanism and stratosphere‐troposphere exchange. Key Points: The Brewer‐Dobson circulation is rising in response to greenhouse gas forcing The rise in the circulation causes an increase in the mass flux at any given pressure level The actual mass exchange between stratosphere and troposphere, however, changes little