Articles | Volume 20, issue 17
https://doi.org/10.5194/acp-20-10531-2020
© Author(s) 2020. 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-20-10531-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
10 Sep 2020
Research article |
| 10 Sep 2020
| 10 Sep 2020
The effect of interactive ozone chemistry on weak and strong stratospheric polar vortex events
Jessica Oehrlein
CORRESPONDING AUTHOR
Department of Applied Physics & Applied Mathematics, Columbia University, New York, United States
Gabriel Chiodo
Department of Applied Physics & Applied Mathematics, Columbia University, New York, United States
Department of Environmental Systems Science, Institute for Atmospheric and Climate Science, ETH Zurich, Zurich, Switzerland
Lorenzo M. Polvani
Department of Applied Physics & Applied Mathematics, Columbia University, New York, United States
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Cited
24 citations as recorded by crossref.
- Influence of Ozone Forcing on 21st Century Southern Hemisphere Surface Westerlies in CMIP6 Models L. Revell et al. 10.1029/2022GL098252
- Atmosphere–ocean–aerosol–chemistry–climate model SOCOLv4.0: description and evaluation T. Sukhodolov et al. 10.5194/gmd-14-5525-2021
- On the additivity of climate responses to the volcanic and solar forcing in the early 19th century S. Fang et al. 10.5194/esd-13-1535-2022
- Ozone‐Forced Southern Annular Mode During Antarctic Stratospheric Warming Events M. Jucker & R. Goyal 10.1029/2021GL095270
- Evaluating Long-Term Variability of the Arctic Stratospheric Polar Vortex Simulated by CMIP6 Models S. Zhao et al. 10.3390/rs14194701
- Exploring the link between austral stratospheric polar vortex anomalies and surface climate in chemistry-climate models N. Bergner et al. 10.5194/acp-22-13915-2022
- Enhanced Climate Response to Ozone Depletion From Ozone‐Circulation Coupling P. Lin & Y. Ming 10.1029/2020JD034286
- Comparison of Arctic and Antarctic Stratospheric Climates in Chemistry Versus No‐Chemistry Climate Models O. Morgenstern et al. 10.1029/2022JD037123
- The Atlantic Jet Response to Stratospheric Events: A Regime Perspective M. Goss et al. 10.1029/2020JD033358
- 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
- Springtime arctic ozone depletion forces northern hemisphere climate anomalies M. Friedel et al. 10.1038/s41561-022-00974-7
- Simulation of Stratospheric Processes with the SLAV072L96 Atmospheric General Circulation Model V. Shashkin et al. 10.3103/S1068373923060018
- How Well Do We Know the Surface Impact of Sudden Stratospheric Warmings? J. Oehrlein et al. 10.1029/2021GL095493
- Stratospheric dynamics modulates ozone layer response to molecular oxygen variations I. Józefiak et al. 10.3389/feart.2023.1239325
- Polar Vortex Multi-Day Intensity Prediction Relying on New Deep Learning Model: A Combined Convolution Neural Network with Long Short-Term Memory Based on Gaussian Smoothing Method K. Peng et al. 10.3390/e23101314
- Long-range prediction and the stratosphere A. Scaife et al. 10.5194/acp-22-2601-2022
- Stratospheric influence on the winter North Atlantic storm track in subseasonal reforecasts H. Afargan-Gerstman et al. 10.5194/wcd-5-231-2024
- Effects of prescribed CMIP6 ozone on simulating the Southern Hemisphere atmospheric circulation response to ozone depletion I. Ivanciu et al. 10.5194/acp-21-5777-2021
- Effects of Arctic ozone on the stratospheric spring onset and its surface impact M. Friedel et al. 10.5194/acp-22-13997-2022
- ACCESS-CM2-Chem: evaluation of southern hemisphere ozone and its effect on the Southern Annular Mode F. Dennison et al. 10.1071/ES22015
- Technical note: Unsupervised classification of ozone profiles in UKESM1 F. Fahrin et al. 10.5194/acp-23-3609-2023
- How Do Stratospheric Perturbations Influence North American Weather Regime Predictions? S. Lee et al. 10.1175/JCLI-D-21-0413.1
- Weakening of springtime Arctic ozone depletion with climate change M. Friedel et al. 10.5194/acp-23-10235-2023
24 citations as recorded by crossref.
- Influence of Ozone Forcing on 21st Century Southern Hemisphere Surface Westerlies in CMIP6 Models L. Revell et al. 10.1029/2022GL098252
- Atmosphere–ocean–aerosol–chemistry–climate model SOCOLv4.0: description and evaluation T. Sukhodolov et al. 10.5194/gmd-14-5525-2021
- On the additivity of climate responses to the volcanic and solar forcing in the early 19th century S. Fang et al. 10.5194/esd-13-1535-2022
- Ozone‐Forced Southern Annular Mode During Antarctic Stratospheric Warming Events M. Jucker & R. Goyal 10.1029/2021GL095270
- Evaluating Long-Term Variability of the Arctic Stratospheric Polar Vortex Simulated by CMIP6 Models S. Zhao et al. 10.3390/rs14194701
- Exploring the link between austral stratospheric polar vortex anomalies and surface climate in chemistry-climate models N. Bergner et al. 10.5194/acp-22-13915-2022
- Enhanced Climate Response to Ozone Depletion From Ozone‐Circulation Coupling P. Lin & Y. Ming 10.1029/2020JD034286
- Comparison of Arctic and Antarctic Stratospheric Climates in Chemistry Versus No‐Chemistry Climate Models O. Morgenstern et al. 10.1029/2022JD037123
- The Atlantic Jet Response to Stratospheric Events: A Regime Perspective M. Goss et al. 10.1029/2020JD033358
- 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
- Springtime arctic ozone depletion forces northern hemisphere climate anomalies M. Friedel et al. 10.1038/s41561-022-00974-7
- Simulation of Stratospheric Processes with the SLAV072L96 Atmospheric General Circulation Model V. Shashkin et al. 10.3103/S1068373923060018
- How Well Do We Know the Surface Impact of Sudden Stratospheric Warmings? J. Oehrlein et al. 10.1029/2021GL095493
- Stratospheric dynamics modulates ozone layer response to molecular oxygen variations I. Józefiak et al. 10.3389/feart.2023.1239325
- Polar Vortex Multi-Day Intensity Prediction Relying on New Deep Learning Model: A Combined Convolution Neural Network with Long Short-Term Memory Based on Gaussian Smoothing Method K. Peng et al. 10.3390/e23101314
- Long-range prediction and the stratosphere A. Scaife et al. 10.5194/acp-22-2601-2022
- Stratospheric influence on the winter North Atlantic storm track in subseasonal reforecasts H. Afargan-Gerstman et al. 10.5194/wcd-5-231-2024
- Effects of prescribed CMIP6 ozone on simulating the Southern Hemisphere atmospheric circulation response to ozone depletion I. Ivanciu et al. 10.5194/acp-21-5777-2021
- Effects of Arctic ozone on the stratospheric spring onset and its surface impact M. Friedel et al. 10.5194/acp-22-13997-2022
- ACCESS-CM2-Chem: evaluation of southern hemisphere ozone and its effect on the Southern Annular Mode F. Dennison et al. 10.1071/ES22015
- Technical note: Unsupervised classification of ozone profiles in UKESM1 F. Fahrin et al. 10.5194/acp-23-3609-2023
- How Do Stratospheric Perturbations Influence North American Weather Regime Predictions? S. Lee et al. 10.1175/JCLI-D-21-0413.1
- Weakening of springtime Arctic ozone depletion with climate change M. Friedel et al. 10.5194/acp-23-10235-2023
Latest update: 26 Apr 2024
Short summary
Winter winds in the stratosphere 10–50 km above the surface impact climate at the surface. Prior studies suggest that this interaction between the stratosphere and the surface is affected by ozone. We compare two ways of including ozone in computer simulations of climate. One method is more realistic but more expensive. We find that the method of including ozone in simulations affects the surface climate when the stratospheric winds are unusually weak but not when they are unusually strong.
Winter winds in the stratosphere 10–50 km above the surface impact climate at the surface....
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