Articles | Volume 22, issue 8
https://doi.org/10.5194/acp-22-5435-2022
© Author(s) 2022. 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-22-5435-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Analyzing ozone variations and uncertainties at high latitudes during sudden stratospheric warming events using MERRA-2
Shima Bahramvash Shams
CORRESPONDING AUTHOR
Department of Civil and Environmental Engineering, Washington State University, Pullman, WA, United States
NCAR, National Center for Atmospheric Research, Boulder, CO, United
States
Von P. Walden
Department of Civil and Environmental Engineering, Washington State University, Pullman, WA, United States
James W. Hannigan
NCAR, National Center for Atmospheric Research, Boulder, CO, United
States
William J. Randel
NCAR, National Center for Atmospheric Research, Boulder, CO, United
States
Irina V. Petropavlovskikh
Cooperative Institute for Research in Environmental Sciences,
University of Colorado, Boulder, CO, USA
National Oceanic and Atmospheric Administration, Global Monitoring
Division, Boulder, CO, USA
Amy H. Butler
National Oceanic and Atmospheric Administration, Chemical Sciences
Laboratory, Boulder, CO, USA
Alvaro de la Cámara
Dept. Física de la Tierra y Astrofísica, Universidad
Complutense de Madrid, Madrid, Spain
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- Air quality and radiative impacts of downward-propagating sudden stratospheric warmings (SSWs) R. Williams et al. 10.5194/acp-24-1389-2024
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Latest update: 24 Dec 2024
Short summary
Large-scale atmospheric circulation has a strong influence on ozone in the Arctic, and certain anomalous dynamical events, such as sudden stratospheric warmings, cause dramatic alterations of the large-scale circulation. A reanalysis model is evaluated and then used to investigate the impact of sudden stratospheric warmings on mid-atmospheric ozone. Results show that the position of the cold jet stream over the Arctic before these events influences the variability of ozone.
Large-scale atmospheric circulation has a strong influence on ozone in the Arctic, and certain...
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