Articles | Volume 39, issue 2
https://doi.org/10.5194/angeo-39-357-2021
© 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/angeo-39-357-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Modelling the residual mean meridional circulation at different stages of sudden stratospheric warming events
Andrey V. Koval
CORRESPONDING AUTHOR
Atmospheric Physics Department, Saint Petersburg State University,
Saint Petersburg 198504, Russia
Department of Meteorological Forecasts, Russian State
Hydrometeorological University, Saint Petersburg 192007, Russia
Wen Chen
Center for Monsoon System Research, Institute of Atmospheric Physics,
Chinese Academy of Sciences, Beijing 100029, PR China
Ksenia A. Didenko
Atmospheric Physics Department, Saint Petersburg State University,
Saint Petersburg 198504, Russia
Department of Meteorological Forecasts, Russian State
Hydrometeorological University, Saint Petersburg 192007, Russia
Tatiana S. Ermakova
Atmospheric Physics Department, Saint Petersburg State University,
Saint Petersburg 198504, Russia
Department of Meteorological Forecasts, Russian State
Hydrometeorological University, Saint Petersburg 192007, Russia
Nikolai M. Gavrilov
Atmospheric Physics Department, Saint Petersburg State University,
Saint Petersburg 198504, Russia
Alexander I. Pogoreltsev
Atmospheric Physics Department, Saint Petersburg State University,
Saint Petersburg 198504, Russia
Department of Meteorological Forecasts, Russian State
Hydrometeorological University, Saint Petersburg 192007, Russia
Olga N. Toptunova
Atmospheric Physics Department, Saint Petersburg State University,
Saint Petersburg 198504, Russia
Department of Meteorological Forecasts, Russian State
Hydrometeorological University, Saint Petersburg 192007, Russia
Ke Wei
Center for Monsoon System Research, Institute of Atmospheric Physics,
Chinese Academy of Sciences, Beijing 100029, PR China
Anna N. Yarusova
Atmospheric Physics Department, Saint Petersburg State University,
Saint Petersburg 198504, Russia
Anton S. Zarubin
Atmospheric Physics Department, Saint Petersburg State University,
Saint Petersburg 198504, Russia
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Cited
18 citations as recorded by crossref.
- Observation and simulation of neutral air density in the middle atmosphere during the 2021 sudden stratospheric warming event J. Yang et al. 10.5194/acp-24-10113-2024
- Numerical Simulation of QBO and ENSO Phase Effect on the Propagation of Planetary Waves and the Evolvement of Sudden Stratospheric Warming V. Lifar et al. 10.1134/S1024856024700489
- Modeling Residual Meridional Circulation at Different Phases of the Quasi-Biennial Oscillation A. Koval et al. 10.1134/S0001433822010054
- Intriguing Aspects of Polar-to-Tropical Mesospheric Teleconnections during the 2018 SSW: A Meteor Radar Network Study S. Eswaraiah et al. 10.3390/atmos14081302
- Observation of vertical coupling during a major sudden stratospheric warming by ICON and GOLD: a case study of the 2020/2021 warming event E. Yiğit et al. 10.3389/fspas.2024.1384196
- Numerical simulation of stratospheric QBO impact on the planetary waves up to the thermosphere A. Koval et al. 10.1038/s41598-022-26311-x
- Long-Term Variations in Parameters of Sudden Stratospheric Warmings According to ERA5 Reanalysis Data O. Zorkaltseva et al. 10.1134/S1024856023040206
- Advances in the Researches of the Middle and Upper Atmosphere in China in 2020–2022 Z. CHEN et al. 10.11728/cjss2022.04.yg20
- Variations of Planetary Wave Activity in the Lower Stratosphere in February as a Predictor of Ozone Depletion in the Arctic in March P. Vargin et al. 10.3390/atmos15101237
- Manifestations of Different El Niño Types in the Dynamics of the Extratropical Stratosphere T. Ermakova et al. 10.3390/atmos13122111
- Changes in general circulation of the middle and upper atmosphere associated with main and transitional QBO phases A. Koval et al. 10.1016/j.asr.2024.07.037
- Anthropogenic Influence on the Antarctic Mesospheric Cooling Observed during the Southern Hemisphere Minor Sudden Stratospheric Warming S. Eswaraiah et al. 10.3390/atmos13091475
- Influence of Natural Tropical Oscillations on Ozone Content and Meridional Circulation in the Boreal Winter Stratosphere T. Ermakova et al. 10.3390/atmos15060717
- Large-scale dynamic processes during the minor and major sudden stratospheric warming events in January–February 2023 P. Vargin et al. 10.1016/j.atmosres.2024.107545
- Dynamical Impacts of Stratospheric QBO on the Global Circulation up to the Lower Thermosphere A. Koval et al. 10.1029/2021JD036095
- Arctic stratosphere changes in the 21st century in the Earth system model SOCOLv4 P. Vargin et al. 10.3389/feart.2023.1214418
- Polar Stratosphere Dynamics During Early Sudden Stratospheric Warmings A. Okulicheva & T. Ermakova 10.1134/S1024856024700702
- Arctic Stratosphere Dynamical Processes in the Winter 2021–2022 P. Vargin et al. 10.3390/atmos13101550
18 citations as recorded by crossref.
- Observation and simulation of neutral air density in the middle atmosphere during the 2021 sudden stratospheric warming event J. Yang et al. 10.5194/acp-24-10113-2024
- Numerical Simulation of QBO and ENSO Phase Effect on the Propagation of Planetary Waves and the Evolvement of Sudden Stratospheric Warming V. Lifar et al. 10.1134/S1024856024700489
- Modeling Residual Meridional Circulation at Different Phases of the Quasi-Biennial Oscillation A. Koval et al. 10.1134/S0001433822010054
- Intriguing Aspects of Polar-to-Tropical Mesospheric Teleconnections during the 2018 SSW: A Meteor Radar Network Study S. Eswaraiah et al. 10.3390/atmos14081302
- Observation of vertical coupling during a major sudden stratospheric warming by ICON and GOLD: a case study of the 2020/2021 warming event E. Yiğit et al. 10.3389/fspas.2024.1384196
- Numerical simulation of stratospheric QBO impact on the planetary waves up to the thermosphere A. Koval et al. 10.1038/s41598-022-26311-x
- Long-Term Variations in Parameters of Sudden Stratospheric Warmings According to ERA5 Reanalysis Data O. Zorkaltseva et al. 10.1134/S1024856023040206
- Advances in the Researches of the Middle and Upper Atmosphere in China in 2020–2022 Z. CHEN et al. 10.11728/cjss2022.04.yg20
- Variations of Planetary Wave Activity in the Lower Stratosphere in February as a Predictor of Ozone Depletion in the Arctic in March P. Vargin et al. 10.3390/atmos15101237
- Manifestations of Different El Niño Types in the Dynamics of the Extratropical Stratosphere T. Ermakova et al. 10.3390/atmos13122111
- Changes in general circulation of the middle and upper atmosphere associated with main and transitional QBO phases A. Koval et al. 10.1016/j.asr.2024.07.037
- Anthropogenic Influence on the Antarctic Mesospheric Cooling Observed during the Southern Hemisphere Minor Sudden Stratospheric Warming S. Eswaraiah et al. 10.3390/atmos13091475
- Influence of Natural Tropical Oscillations on Ozone Content and Meridional Circulation in the Boreal Winter Stratosphere T. Ermakova et al. 10.3390/atmos15060717
- Large-scale dynamic processes during the minor and major sudden stratospheric warming events in January–February 2023 P. Vargin et al. 10.1016/j.atmosres.2024.107545
- Dynamical Impacts of Stratospheric QBO on the Global Circulation up to the Lower Thermosphere A. Koval et al. 10.1029/2021JD036095
- Arctic stratosphere changes in the 21st century in the Earth system model SOCOLv4 P. Vargin et al. 10.3389/feart.2023.1214418
- Polar Stratosphere Dynamics During Early Sudden Stratospheric Warmings A. Okulicheva & T. Ermakova 10.1134/S1024856024700702
- Arctic Stratosphere Dynamical Processes in the Winter 2021–2022 P. Vargin et al. 10.3390/atmos13101550
Latest update: 26 Dec 2024
Short summary
Numerical modelling is used to simulate atmospheric circulation and calculate residual mean meridional circulation (RMC) during sudden stratospheric warming (SSW) events. Calculating the RMC is used to take into account wave effects on the transport of atmospheric quantities and gas species in the meridional plane. The results show that RMC undergoes significant changes at different stages of SSW and contributes to SSW development.
Numerical modelling is used to simulate atmospheric circulation and calculate residual mean...