Articles | Volume 2, issue 2
https://doi.org/10.5194/wcd-2-453-2021
© 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/wcd-2-453-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
27 May 2021
Research article |
| 27 May 2021
| 27 May 2021
The wave geometry of final stratospheric warming events
Chemical Sciences Laboratory, National Oceanic and Atmospheric Administration, Boulder, CO, USA
Daniela I. V. Domeisen
Institute for Atmospheric and Climate Science, ETH Zürich, Zurich, Switzerland
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Cited
18 citations as recorded by crossref.
- Interannual Variability of Stratospheric Final Warming in the Southern Hemisphere and Its Tropospheric Origin S. Hirano et al. 10.1175/JCLI-D-20-0945.1
- Classification of Stratosphere Winter Evolutions Into Four Different Scenarios in the Northern Hemisphere A. Mariaccia et al. 10.1029/2022JD036662
- Dynamics of ENSO-driven stratosphere-to-troposphere transport of ozone over North America J. Albers et al. 10.5194/acp-22-13035-2022
- Response of quasi-10-day waves in the MLT region to the sudden stratospheric warming in March 2020 S. Yin et al. 10.1016/j.asr.2022.10.054
- Stratospheric influence on the winter North Atlantic storm track in subseasonal reforecasts H. Afargan-Gerstman et al. 10.5194/wcd-5-231-2024
- Rossby Waves in Total Ozone over the Arctic in 2000–2021 C. Zhang et al. 10.3390/rs14092192
- Effects of Arctic ozone on the stratospheric spring onset and its surface impact M. Friedel et al. 10.5194/acp-22-13997-2022
- 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
- The influence of future changes in springtime Arctic ozone on stratospheric and surface climate G. Chiodo et al. 10.5194/acp-23-10451-2023
- Quantifying stratospheric biases and identifying their potential sources in subseasonal forecast systems Z. Lawrence et al. 10.5194/wcd-3-977-2022
- Preconditioned Stratospheric Modulation on the Occurrence of Stratospheric Final Warmings P. Yang et al. 10.1029/2023GL107294
- Analyzing ozone variations and uncertainties at high latitudes during sudden stratospheric warming events using MERRA-2 S. Bahramvash Shams et al. 10.5194/acp-22-5435-2022
- Differences in the sub-seasonal predictability of extreme stratospheric events R. Wu et al. 10.5194/wcd-3-755-2022
- Antarctic planetary wave spectrum under different polar vortex conditions in 2019 and 2020 based on total ozone column data А. Grytsai et al. 10.33275/1727-7485.1.2022.687
- Enhanced Polar Vortex Predictability Following Sudden Stratospheric Warming Events P. Rupp et al. 10.1029/2023GL104057
- First Observational Evidence for the Role of Polar Vortex Strength in Modulating the Activity of Planetary Waves in the MLT Region Z. Ma et al. 10.1029/2021GL096548
- Warmer Antarctic summers in recent decades linked to earlier stratospheric final warming occurrences H. Choi et al. 10.1038/s43247-024-01221-0
- Stratospheric Final Warmings fall into two categories with different evolution over the course of the year A. Hauchecorne et al. 10.1038/s43247-021-00335-z
17 citations as recorded by crossref.
- Interannual Variability of Stratospheric Final Warming in the Southern Hemisphere and Its Tropospheric Origin S. Hirano et al. 10.1175/JCLI-D-20-0945.1
- Classification of Stratosphere Winter Evolutions Into Four Different Scenarios in the Northern Hemisphere A. Mariaccia et al. 10.1029/2022JD036662
- Dynamics of ENSO-driven stratosphere-to-troposphere transport of ozone over North America J. Albers et al. 10.5194/acp-22-13035-2022
- Response of quasi-10-day waves in the MLT region to the sudden stratospheric warming in March 2020 S. Yin et al. 10.1016/j.asr.2022.10.054
- Stratospheric influence on the winter North Atlantic storm track in subseasonal reforecasts H. Afargan-Gerstman et al. 10.5194/wcd-5-231-2024
- Rossby Waves in Total Ozone over the Arctic in 2000–2021 C. Zhang et al. 10.3390/rs14092192
- Effects of Arctic ozone on the stratospheric spring onset and its surface impact M. Friedel et al. 10.5194/acp-22-13997-2022
- 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
- The influence of future changes in springtime Arctic ozone on stratospheric and surface climate G. Chiodo et al. 10.5194/acp-23-10451-2023
- Quantifying stratospheric biases and identifying their potential sources in subseasonal forecast systems Z. Lawrence et al. 10.5194/wcd-3-977-2022
- Preconditioned Stratospheric Modulation on the Occurrence of Stratospheric Final Warmings P. Yang et al. 10.1029/2023GL107294
- Analyzing ozone variations and uncertainties at high latitudes during sudden stratospheric warming events using MERRA-2 S. Bahramvash Shams et al. 10.5194/acp-22-5435-2022
- Differences in the sub-seasonal predictability of extreme stratospheric events R. Wu et al. 10.5194/wcd-3-755-2022
- Antarctic planetary wave spectrum under different polar vortex conditions in 2019 and 2020 based on total ozone column data А. Grytsai et al. 10.33275/1727-7485.1.2022.687
- Enhanced Polar Vortex Predictability Following Sudden Stratospheric Warming Events P. Rupp et al. 10.1029/2023GL104057
- First Observational Evidence for the Role of Polar Vortex Strength in Modulating the Activity of Planetary Waves in the MLT Region Z. Ma et al. 10.1029/2021GL096548
- Warmer Antarctic summers in recent decades linked to earlier stratospheric final warming occurrences H. Choi et al. 10.1038/s43247-024-01221-0
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Short summary
We classify by wave geometry the stratospheric polar vortex during the final warming that occurs every spring in both hemispheres due to a combination of radiative and dynamical processes. We show that the shape of the vortex, as well as the timing of the seasonal transition, is linked to total column ozone prior to and surface weather following the final warming. These results have implications for prediction and our understanding of stratosphere–troposphere coupling processes in springtime.
We classify by wave geometry the stratospheric polar vortex during the final warming that occurs...
