Articles | Volume 17, issue 2
https://doi.org/10.5194/acp-17-1313-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/acp-17-1313-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Time-varying changes in the simulated structure of the Brewer–Dobson Circulation
Chaim I. Garfinkel
CORRESPONDING AUTHOR
The Fredy and Nadine Herrmann Institute of Earth Sciences, Hebrew University, Jerusalem, Israel
Valentina Aquila
Department of Earth and Planetary Science, Johns Hopkins University, Baltimore, MD, USA
Goddard Earth Science Technology and Research, Greenbelt, MD, USA
NASA Goddard Space Flight Center, Greenbelt, MD, USA
Darryn W. Waugh
Department of Earth and Planetary Science, Johns Hopkins University, Baltimore, MD, USA
Luke D. Oman
NASA Goddard Space Flight Center, Greenbelt, MD, USA
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- Significant Contributions of Volcanic Aerosols to Decadal Changes in the Stratospheric Circulation M. Diallo et al. 10.1002/2017GL074662
- The Impact of Ozone-Depleting Substances on Tropical Upwelling, as Revealed by the Absence of Lower-Stratospheric Cooling since the Late 1990s L. Polvani et al. 10.1175/JCLI-D-16-0532.1
- The Influence of Internal Climate Variability on Stratospheric Water Vapor Increases After Large‐Magnitude Explosive Tropical Volcanic Eruptions X. Zhou et al. 10.1029/2023GL103076
- Mechanisms Linked to Recent Ozone Decreases in the Northern Hemisphere Lower Stratosphere C. Orbe et al. 10.1029/2019JD031631
- Indirect stratospheric moisture increase after a Pinatubo-magnitude eruption can be comparable to direct increase after 2022 Hunga C. Kroll & A. Schmidt 10.1038/s43247-024-01651-w
- Impact of Stratospheric Volcanic Aerosols on Age-of-Air and Transport of Long-Lived Species G. Pitari et al. 10.3390/atmos7110149
25 citations as recorded by crossref.
- The Unusual Stratospheric Arctic Winter 2019/20: Chemical Ozone Loss From Satellite Observations and TOMCAT Chemical Transport Model M. Weber et al. 10.1029/2020JD034386
- Resolving the 21st century temperature trends of the upper troposphere–lower stratosphere with satellite observations F. Ladstädter et al. 10.1038/s41598-023-28222-x
- Effects of Greenhouse Gas Increase and Stratospheric Ozone Depletion on Stratospheric Mean Age of Air in 1960–2010 F. Li et al. 10.1002/2017JD027562
- Large Impacts, Past and Future, of Ozone‐Depleting Substances on Brewer‐Dobson Circulation Trends: A Multimodel Assessment L. Polvani et al. 10.1029/2018JD029516
- Secular change in atmospheric Ar∕N<sub>2</sub> and its implications for ocean heat uptake and Brewer–Dobson circulation S. Ishidoya et al. 10.5194/acp-21-1357-2021
- New Insights on the Impact of Ozone‐Depleting Substances on the Brewer‐Dobson Circulation M. Abalos et al. 10.1029/2018JD029301
- Shift of subtropical transport barriers explains observed hemispheric asymmetry of decadal trends of age of air G. Stiller et al. 10.5194/acp-17-11177-2017
- Multi-decadal variability controls short-term stratospheric water vapor trends M. Tao et al. 10.1038/s43247-023-01094-9
- Tropical Stratospheric Circulation and Ozone Coupled to Pacific Multi‐Decadal Variability F. Iglesias‐Suarez et al. 10.1029/2020GL092162
- Climate change modulates the stratospheric volcanic sulfate aerosol lifecycle and radiative forcing from tropical eruptions T. Aubry et al. 10.1038/s41467-021-24943-7
- Contributions of Convective and Orographic Gravity Waves to the Brewer–Dobson Circulation Estimated from NCEP CFSR M. Kang et al. 10.1175/JAS-D-19-0177.1
- Climatology and long-term evolution of ozone and carbon monoxide in the upper troposphere–lower stratosphere (UTLS) at northern midlatitudes, as seen by IAGOS from 1995 to 2013 Y. Cohen et al. 10.5194/acp-18-5415-2018
- Nonlinear response of tropical lower-stratospheric temperature and water vapor to ENSO C. Garfinkel et al. 10.5194/acp-18-4597-2018
- Three-dimensional simulation of stratospheric gravitational separation using the NIES global atmospheric tracer transport model D. Belikov et al. 10.5194/acp-19-5349-2019
- Hemispheric asymmetry in stratospheric NO<sub>2</sub> trends M. Yela et al. 10.5194/acp-17-13373-2017
- Comparison of mean age of air in five reanalyses using the BASCOE transport model S. Chabrillat et al. 10.5194/acp-18-14715-2018
- How robust are stratospheric age of air trends from different reanalyses? F. Ploeger et al. 10.5194/acp-19-6085-2019
- The Interactive Stratospheric Aerosol Model Intercomparison Project (ISA-MIP): motivation and experimental design C. Timmreck et al. 10.5194/gmd-11-2581-2018
- The advective Brewer–Dobson circulation in the ERA5 reanalysis: climatology, variability, and trends M. Diallo et al. 10.5194/acp-21-7515-2021
- Why does stratospheric aerosol forcing strongly cool the warm pool? M. Günther et al. 10.5194/acp-24-7203-2024
- Significant Contributions of Volcanic Aerosols to Decadal Changes in the Stratospheric Circulation M. Diallo et al. 10.1002/2017GL074662
- The Impact of Ozone-Depleting Substances on Tropical Upwelling, as Revealed by the Absence of Lower-Stratospheric Cooling since the Late 1990s L. Polvani et al. 10.1175/JCLI-D-16-0532.1
- The Influence of Internal Climate Variability on Stratospheric Water Vapor Increases After Large‐Magnitude Explosive Tropical Volcanic Eruptions X. Zhou et al. 10.1029/2023GL103076
- Mechanisms Linked to Recent Ozone Decreases in the Northern Hemisphere Lower Stratosphere C. Orbe et al. 10.1029/2019JD031631
- Indirect stratospheric moisture increase after a Pinatubo-magnitude eruption can be comparable to direct increase after 2022 Hunga C. Kroll & A. Schmidt 10.1038/s43247-024-01651-w
1 citations as recorded by crossref.
Latest update: 20 Nov 2024
Short summary
Previous work has noted a discrepancy between models and observations in trends of the large-scale overturning circulation in the stratosphere. Here, we show that a model can simulate trends that are reminiscent of those observed, including space- and time-varying trends in different regions of the stratosphere. We therefore clarify that the statement that is often made that models simulate an accelerated circulation only applies over long time periods and is not true for the past 25 years.
Previous work has noted a discrepancy between models and observations in trends of the...
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