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
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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27 citations as recorded by crossref.
- N2O as a regression proxy for dynamical variability in stratospheric trace gas trends K. Dubé et al. 10.5194/acp-23-13283-2023
- Stratosphere‐Troposphere Exchanges of Air Mass and Ozone Concentration in the Last Glacial Maximum M. Wang et al. 10.1029/2021JD036327
- Evaluation of the N2O Rate of Change to Understand the Stratospheric Brewer‐Dobson Circulation in a Chemistry‐Climate Model D. Minganti et al. 10.1029/2021JD036390
- Global biosphere primary productivity changes during the past eight glacial cycles J. Yang et al. 10.1126/science.abj8826
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- Comment on “Observation of large and all-season ozone losses over the tropics” [AIP Adv. 12, 075006 (2022)] M. Chipperfield et al. 10.1063/5.0121723
- Climate, Variability, and Climate Sensitivity of “Middle Atmosphere” Chemistry Configurations of the Community Earth System Model Version 2, Whole Atmosphere Community Climate Model Version 6 (CESM2(WACCM6)) N. Davis et al. 10.1029/2022MS003579
- Observed changes in stratospheric circulation: decreasing lifetime of N2O, 2005–2021 M. Prather et al. 10.5194/acp-23-843-2023
- Influence of stratosphere-troposphere exchange on long-term trends of surface ozone in CMIP6 Y. Li et al. 10.1016/j.atmosres.2023.107086
- HSW-V v1.0: localized injections of interactive volcanic aerosols and their climate impacts in a simple general circulation model J. Hollowed et al. 10.5194/gmd-17-5913-2024
- Analysis of the global atmospheric background sulfur budget in a multi-model framework C. Brodowsky et al. 10.5194/acp-24-5513-2024
- Age of air from in situ trace gas measurements: insights from a new technique E. Ray et al. 10.5194/acp-24-12425-2024
- Stratosphere‐Troposphere Exchanges of Air Mass and Ozone Concentrations From ERA5 and MERRA2: Annual‐Mean Climatology, Seasonal Cycle, and Interannual Variability M. Wang et al. 10.1029/2023JD039270
- 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
- Changes in Stratosphere‐Troposphere Exchange of Air Mass and Ozone Concentration in CCMI Models From 1960 to 2099 M. Wang & Q. Fu 10.1029/2023JD038487
- Injection strategy – a driver of atmospheric circulation and ozone response to stratospheric aerosol geoengineering E. Bednarz et al. 10.5194/acp-23-13665-2023
- Tropospheric Expansion Under Global Warming Reduces Tropical Lower Stratospheric Ozone A. Match & E. Gerber 10.1029/2022GL099463
- Weakening of the tropical tropopause layer cold trap with global warming S. Bourguet & M. Linz 10.5194/acp-23-7447-2023
- The Antarctic contribution to 21st-century sea-level rise predicted by the UK Earth System Model with an interactive ice sheet A. Siahaan et al. 10.5194/tc-16-4053-2022
- The response of the North Pacific jet and stratosphere-to-troposphere transport of ozone over western North America to RCP8.5 climate forcing D. Elsbury et al. 10.5194/acp-23-5101-2023
- Hemispheric asymmetries in recent changes in the stratospheric circulation F. Ploeger & H. Garny 10.5194/acp-22-5559-2022
- Weakening of springtime Arctic ozone depletion with climate change M. Friedel et al. 10.5194/acp-23-10235-2023
- 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
- MAP-IO: an atmospheric and marine observatory program on board Marion Dufresne over the Southern Ocean P. Tulet et al. 10.5194/essd-16-3821-2024
Latest update: 13 Dec 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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