Articles | Volume 14, issue 23
https://doi.org/10.5194/acp-14-12803-2014
© Author(s) 2014. 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-14-12803-2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
On the hiatus in the acceleration of tropical upwelling since the beginning of the 21st century
J. Aschmann
CORRESPONDING AUTHOR
Institute of Environmental Physics, University of Bremen, Bremen, Germany
J. P. Burrows
Institute of Environmental Physics, University of Bremen, Bremen, Germany
C. Gebhardt
Institute of Environmental Physics, University of Bremen, Bremen, Germany
A. Rozanov
Institute of Environmental Physics, University of Bremen, Bremen, Germany
R. Hommel
Institute of Environmental Physics, University of Bremen, Bremen, Germany
Institute of Environmental Physics, University of Bremen, Bremen, Germany
A. M. Thompson
NASA/Goddard Space Flight Center, Greenbelt, MD, USA
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14 citations as recorded by crossref.
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- 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
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- Time-varying changes in the simulated structure of the Brewer–Dobson Circulation C. Garfinkel et al. 10.5194/acp-17-1313-2017
- Variability of stratospheric mean age of air and of the local effects of residual circulation and eddy mixing F. Ploeger et al. 10.1002/2014JD022468
- Is global ozone recovering? W. Steinbrecht et al. 10.1016/j.crte.2018.07.012
- The upward branch of the Brewer‐Dobson circulation quantified by tropical stratospheric water vapor and carbon monoxide measurements from the Aura Microwave Limb Sounder K. Minschwaner et al. 10.1002/2015JD023961
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- Dynamically controlled ozone decline in the tropical mid-stratosphere observed by SCIAMACHY E. Galytska et al. 10.5194/acp-19-767-2019
1 citations as recorded by crossref.
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Latest update: 19 Nov 2024
Short summary
This study compares observations and simulation results of ozone in the lower tropical stratosphere. It shows that ozone in this region decreased from 1985 up to about 2002, which is consistent with an increase in tropical upwelling predicted by climate models. However, the decrease effectively stops after 2002, indicating that significant changes in tropical upwelling have occurred. The most important factor appears to be that the vertical ascent in the tropics is no longer accelerating.
This study compares observations and simulation results of ozone in the lower tropical...
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