Articles | Volume 21, issue 17
https://doi.org/10.5194/acp-21-13571-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/acp-21-13571-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
10 Sep 2021
Research article |
| 10 Sep 2021
| 10 Sep 2021
The Brewer–Dobson circulation in CMIP6
Earth Physics and Astrophysics Department, Universidad Complutense de Madrid, Madrid, Spain
Natalia Calvo
Earth Physics and Astrophysics Department, Universidad Complutense de Madrid, Madrid, Spain
Samuel Benito-Barca
Earth Physics and Astrophysics Department, Universidad Complutense de Madrid, Madrid, Spain
Hella Garny
Deutsches Zentrum für Luft- und Raumfahrt (DLR), Oberpfaffenhofen, Germany
Steven C. Hardiman
Met Office Hadley Centre, Exeter, United Kingdom
Pu Lin
NOAA/Geophysical Fluid Dynamics Laboratory, Princeton, NJ, USA
Program in Atmospheric and Oceanic Sciences, Princeton University, Princeton, NJ, USA
Martin B. Andrews
Met Office Hadley Centre, Exeter, United Kingdom
Neal Butchart
Met Office Hadley Centre, Exeter, United Kingdom
Rolando Garcia
National Center for Atmospheric Research, Boulder, CO, USA
Clara Orbe
NASA Goddard Institute for Space Studies, New York, NY, USA
David Saint-Martin
Centre National de Recherches Météorologiques, Toulouse, France
Shingo Watanabe
Japan Agency for Marine-Earth Science and Technology (JAMSTEC), Yokohama, Japan
Kohei Yoshida
Meteorological Research Institute, Tsukuba, Japan
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- Long-term variability of human health-related solar ultraviolet-B radiation doses from the 1980s to the end of the 21st century C. Zerefos et al. 10.1152/physrev.00031.2022
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- Arctic stratosphere changes in the 21st century in the Earth system model SOCOLv4 P. Vargin et al. 10.3389/feart.2023.1214418
- Arctic Stratosphere Circulation Changes in the 21st Century in Simulations of INM CM5 P. Vargin et al. 10.3390/atmos13010025
- Why the lower stratosphere cools when the troposphere warms J. Lin & K. Emanuel 10.1073/pnas.2319228121
- The impact of different CO2 and ODS levels on the mean state and variability of the springtime Arctic stratosphere J. Kult-Herdin et al. 10.1088/1748-9326/acb0e6
Latest update: 29 Jun 2024
Short summary
The stratospheric Brewer–Dobson circulation (BDC), responsible for transporting mass, tracers and heat globally in the stratosphere, is evaluated in a set of state-of-the-art climate models. The acceleration of the BDC in response to increasing greenhouse gases is most robust in the lower stratosphere. At higher levels, the well-known inconsistency between model and observational BDC trends can be partly reconciled by accounting for limited sampling and large uncertainties in the observations.
The stratospheric Brewer–Dobson circulation (BDC), responsible for transporting mass, tracers...
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