Articles | Volume 23, issue 7
https://doi.org/10.5194/acp-23-4105-2023
© Author(s) 2023. 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-23-4105-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Numerical modelling of relative contribution of planetary waves to the atmospheric circulation
Andrey V. Koval
Atmospheric Physics Department, Saint Petersburg State University,
Saint Petersburg, 199034, Russia
Department of Meteorological Forecasts, Russian State
Hydrometeorological University, Saint Petersburg, 195196, Russia
Olga N. Toptunova
Department of Meteorological Forecasts, Russian State
Hydrometeorological University, Saint Petersburg, 195196, Russia
Maxim A. Motsakov
Department of Meteorological Forecasts, Russian State
Hydrometeorological University, Saint Petersburg, 195196, Russia
Ksenia A. Didenko
Atmospheric Physics Department, Saint Petersburg State University,
Saint Petersburg, 199034, Russia
Department of Meteorological Forecasts, Russian State
Hydrometeorological University, Saint Petersburg, 195196, Russia
Tatiana S. Ermakova
Atmospheric Physics Department, Saint Petersburg State University,
Saint Petersburg, 199034, Russia
Department of Meteorological Forecasts, Russian State
Hydrometeorological University, Saint Petersburg, 195196, Russia
Nikolai M. Gavrilov
Atmospheric Physics Department, Saint Petersburg State University,
Saint Petersburg, 199034, Russia
Eugene V. Rozanov
CORRESPONDING AUTHOR
Physikalisch-Meteorologisches Observatorium, Davos World Radiation
Centre, Davos Dorf, 7260, Switzerland
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The main patterns of tropical oscillations influence on atmospheric planetary waves were investigated by numerical simulation of atmospheric circulation.
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Andrey V. Koval, Wen Chen, Ksenia A. Didenko, Tatiana S. Ermakova, Nikolai M. Gavrilov, Alexander I. Pogoreltsev, Olga N. Toptunova, Ke Wei, Anna N. Yarusova, and Anton S. Zarubin
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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.
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The results showed that the joint effect of the considered tropical oscillations, originating in low latitudes, significantly affect the structure of planetary waves, not only in the regions of their climatic maxima but also throughout the middle atmosphere and thermosphere of both hemispheres.
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Atmos. Chem. Phys., 25, 3623–3634, https://doi.org/10.5194/acp-25-3623-2025, https://doi.org/10.5194/acp-25-3623-2025, 2025
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Miriam Sinnhuber, Christina Arras, Stefan Bender, Bernd Funke, Hanli Liu, Daniel R. Marsh, Thomas Reddmann, Eugene Rozanov, Timofei Sukhodolov, Monika E. Szelag, and Jan Maik Wissing
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Christina V. Brodowsky, Timofei Sukhodolov, Gabriel Chiodo, Valentina Aquila, Slimane Bekki, Sandip S. Dhomse, Michael Höpfner, Anton Laakso, Graham W. Mann, Ulrike Niemeier, Giovanni Pitari, Ilaria Quaglia, Eugene Rozanov, Anja Schmidt, Takashi Sekiya, Simone Tilmes, Claudia Timmreck, Sandro Vattioni, Daniele Visioni, Pengfei Yu, Yunqian Zhu, and Thomas Peter
Atmos. Chem. Phys., 24, 5513–5548, https://doi.org/10.5194/acp-24-5513-2024, https://doi.org/10.5194/acp-24-5513-2024, 2024
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The aerosol layer is an essential part of the climate system. We characterize the sulfur budget in a volcanically quiescent (background) setting, with a special focus on the sulfate aerosol layer using, for the first time, a multi-model approach. The aim is to identify weak points in the representation of the atmospheric sulfur budget in an intercomparison of nine state-of-the-art coupled global circulation models.
Franziska Zilker, Timofei Sukhodolov, Gabriel Chiodo, Marina Friedel, Tatiana Egorova, Eugene Rozanov, Jan Sedlacek, Svenja Seeber, and Thomas Peter
Atmos. Chem. Phys., 23, 13387–13411, https://doi.org/10.5194/acp-23-13387-2023, https://doi.org/10.5194/acp-23-13387-2023, 2023
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The Montreal Protocol (MP) has successfully reduced the Antarctic ozone hole by banning chlorofluorocarbons (CFCs) that destroy the ozone layer. Moreover, CFCs are strong greenhouse gases (GHGs) that would have strengthened global warming. In this study, we investigate the surface weather and climate in a world without the MP at the end of the 21st century, disentangling ozone-mediated and GHG impacts of CFCs. Overall, we avoided 1.7 K global surface warming and a poleward shift in storm tracks.
Marina Friedel, Gabriel Chiodo, Timofei Sukhodolov, James Keeble, Thomas Peter, Svenja Seeber, Andrea Stenke, Hideharu Akiyoshi, Eugene Rozanov, David Plummer, Patrick Jöckel, Guang Zeng, Olaf Morgenstern, and Béatrice Josse
Atmos. Chem. Phys., 23, 10235–10254, https://doi.org/10.5194/acp-23-10235-2023, https://doi.org/10.5194/acp-23-10235-2023, 2023
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Previously, it has been suggested that springtime Arctic ozone depletion might worsen in the coming decades due to climate change, which might counteract the effect of reduced ozone-depleting substances. Here, we show with different chemistry–climate models that springtime Arctic ozone depletion will likely decrease in the future. Further, we explain why models show a large spread in the projected development of Arctic ozone depletion and use the model spread to constrain future projections.
Tatiana Egorova, Jan Sedlacek, Timofei Sukhodolov, Arseniy Karagodin-Doyennel, Franziska Zilker, and Eugene Rozanov
Atmos. Chem. Phys., 23, 5135–5147, https://doi.org/10.5194/acp-23-5135-2023, https://doi.org/10.5194/acp-23-5135-2023, 2023
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This paper describes the climate and atmosphere benefits of the Montreal Protocol, simulated with the state-of-the-art Earth system model SOCOLv4.0. We have added to and confirmed the previous studies by showing that without the Montreal Protocol by the end of the 21st century there would be a dramatic reduction in the ozone layer as well as substantial perturbation of the essential climate variables in the troposphere caused by the warming from increasing ozone-depleting substances.
Arseniy Karagodin-Doyennel, Eugene Rozanov, Timofei Sukhodolov, Tatiana Egorova, Jan Sedlacek, and Thomas Peter
Atmos. Chem. Phys., 23, 4801–4817, https://doi.org/10.5194/acp-23-4801-2023, https://doi.org/10.5194/acp-23-4801-2023, 2023
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The future ozone evolution in SOCOLv4 simulations under SSP2-4.5 and SSP5-8.5 scenarios has been assessed for the period 2015–2099 and subperiods using the DLM approach. The SOCOLv4 projects a decline in tropospheric ozone in the 2030s in SSP2-4.5 and in the 2060s in SSP5-8.5. The stratospheric ozone increase is ~3 times higher in SSP5-8.5, confirming the important role of GHGs in ozone evolution. We also showed that tropospheric ozone strongly impacts the total column in the tropics.
Ilaria Quaglia, Claudia Timmreck, Ulrike Niemeier, Daniele Visioni, Giovanni Pitari, Christina Brodowsky, Christoph Brühl, Sandip S. Dhomse, Henning Franke, Anton Laakso, Graham W. Mann, Eugene Rozanov, and Timofei Sukhodolov
Atmos. Chem. Phys., 23, 921–948, https://doi.org/10.5194/acp-23-921-2023, https://doi.org/10.5194/acp-23-921-2023, 2023
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The last very large explosive volcanic eruption we have measurements for is the eruption of Mt. Pinatubo in 1991. It is therefore often used as a benchmark for climate models' ability to reproduce these kinds of events. Here, we compare available measurements with the results from multiple experiments conducted with climate models interactively simulating the aerosol cloud formation.
Arseniy Karagodin-Doyennel, Eugene Rozanov, Timofei Sukhodolov, Tatiana Egorova, Jan Sedlacek, William Ball, and Thomas Peter
Atmos. Chem. Phys., 22, 15333–15350, https://doi.org/10.5194/acp-22-15333-2022, https://doi.org/10.5194/acp-22-15333-2022, 2022
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Applying the dynamic linear model, we confirm near-global ozone recovery (55°N–55°S) in the mesosphere, upper and middle stratosphere, and a steady increase in the troposphere. We also show that modern chemistry–climate models (CCMs) like SOCOLv4 may reproduce the observed trend distribution of lower stratospheric ozone, despite exhibiting a lower magnitude and statistical significance. The obtained ozone trend pattern in SOCOLv4 is generally consistent with observations and reanalysis datasets.
Nikolai M. Gavrilov, Sergey P. Kshevetskii, and Andrey V. Koval
Atmos. Chem. Phys., 22, 13713–13724, https://doi.org/10.5194/acp-22-13713-2022, https://doi.org/10.5194/acp-22-13713-2022, 2022
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We make high-resolution simulations of poorly understood decays of nonlinear atmospheric acoustic–gravity waves (AGWs) after deactivations of the wave forcing. The standard deviations of AGW perturbations, after fast dispersions of traveling modes, experience slower exponential decreases. AGW decay times are estimated for the first time and are 20–100 h in the stratosphere and mesosphere. This requires slow, quasi-standing and secondary modes in parameterizations of AGW impacts to be considered.
Irina Mironova, Miriam Sinnhuber, Galina Bazilevskaya, Mark Clilverd, Bernd Funke, Vladimir Makhmutov, Eugene Rozanov, Michelle L. Santee, Timofei Sukhodolov, and Thomas Ulich
Atmos. Chem. Phys., 22, 6703–6716, https://doi.org/10.5194/acp-22-6703-2022, https://doi.org/10.5194/acp-22-6703-2022, 2022
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From balloon measurements, we detected unprecedented, extremely powerful, electron precipitation over the middle latitudes. The robustness of this event is confirmed by satellite observations of electron fluxes and chemical composition, as well as by ground-based observations of the radio signal propagation. The applied chemistry–climate model shows the almost complete destruction of ozone in the mesosphere over the region where high-energy electrons were observed.
Kseniia Golubenko, Eugene Rozanov, Gennady Kovaltsov, Ari-Pekka Leppänen, Timofei Sukhodolov, and Ilya Usoskin
Geosci. Model Dev., 14, 7605–7620, https://doi.org/10.5194/gmd-14-7605-2021, https://doi.org/10.5194/gmd-14-7605-2021, 2021
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A new full 3-D time-dependent model, based on SOCOL-AERv2, of beryllium atmospheric production, transport, and deposition has been developed and validated using directly measured data. The model is recommended to be used in studies related to, e.g., atmospheric dynamical patterns, extreme solar particle storms, long-term solar activity reconstruction from cosmogenic proxy data, and solar–terrestrial relations.
Arseniy Karagodin-Doyennel, Eugene Rozanov, Timofei Sukhodolov, Tatiana Egorova, Alfonso Saiz-Lopez, Carlos A. Cuevas, Rafael P. Fernandez, Tomás Sherwen, Rainer Volkamer, Theodore K. Koenig, Tanguy Giroud, and Thomas Peter
Geosci. Model Dev., 14, 6623–6645, https://doi.org/10.5194/gmd-14-6623-2021, https://doi.org/10.5194/gmd-14-6623-2021, 2021
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Here, we present the iodine chemistry module in the SOCOL-AERv2 model. The obtained iodine distribution demonstrated a good agreement when validated against other simulations and available observations. We also estimated the iodine influence on ozone in the case of present-day iodine emissions, the sensitivity of ozone to doubled iodine emissions, and when considering only organic or inorganic iodine sources. The new model can be used as a tool for further studies of iodine effects on ozone.
Timofei Sukhodolov, Tatiana Egorova, Andrea Stenke, William T. Ball, Christina Brodowsky, Gabriel Chiodo, Aryeh Feinberg, Marina Friedel, Arseniy Karagodin-Doyennel, Thomas Peter, Jan Sedlacek, Sandro Vattioni, and Eugene Rozanov
Geosci. Model Dev., 14, 5525–5560, https://doi.org/10.5194/gmd-14-5525-2021, https://doi.org/10.5194/gmd-14-5525-2021, 2021
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This paper features the new atmosphere–ocean–aerosol–chemistry–climate model SOCOLv4.0 and its validation. The model performance is evaluated against reanalysis products and observations of atmospheric circulation and trace gas distribution, with a focus on stratospheric processes. Although we identified some problems to be addressed in further model upgrades, we demonstrated that SOCOLv4.0 is already well suited for studies related to chemistry–climate–aerosol interactions.
Andrey V. Koval, Wen Chen, Ksenia A. Didenko, Tatiana S. Ermakova, Nikolai M. Gavrilov, Alexander I. Pogoreltsev, Olga N. Toptunova, Ke Wei, Anna N. Yarusova, and Anton S. Zarubin
Ann. Geophys., 39, 357–368, https://doi.org/10.5194/angeo-39-357-2021, https://doi.org/10.5194/angeo-39-357-2021, 2021
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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.
Margot Clyne, Jean-Francois Lamarque, Michael J. Mills, Myriam Khodri, William Ball, Slimane Bekki, Sandip S. Dhomse, Nicolas Lebas, Graham Mann, Lauren Marshall, Ulrike Niemeier, Virginie Poulain, Alan Robock, Eugene Rozanov, Anja Schmidt, Andrea Stenke, Timofei Sukhodolov, Claudia Timmreck, Matthew Toohey, Fiona Tummon, Davide Zanchettin, Yunqian Zhu, and Owen B. Toon
Atmos. Chem. Phys., 21, 3317–3343, https://doi.org/10.5194/acp-21-3317-2021, https://doi.org/10.5194/acp-21-3317-2021, 2021
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This study finds how and why five state-of-the-art global climate models with interactive stratospheric aerosols differ when simulating the aftermath of large volcanic injections as part of the Model Intercomparison Project on the climatic response to Volcanic forcing (VolMIP). We identify and explain the consequences of significant disparities in the underlying physics and chemistry currently in some of the models, which are problems likely not unique to the models participating in this study.
Sergei P. Smyshlyaev, Pavel N. Vargin, Alexander N. Lukyanov, Natalia D. Tsvetkova, and Maxim A. Motsakov
Atmos. Chem. Phys. Discuss., https://doi.org/10.5194/acp-2021-11, https://doi.org/10.5194/acp-2021-11, 2021
Revised manuscript not accepted
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The dynamical processes and changes in Arctic ozone during the winter-spring season 2019–2020 were analyzed using ozonesondes, reanalysis data and numerical experiments with chemistry-transport and trajectory models. The results of numerical experiments indicated that dynamical processes predominate in ozone loss, and the chemical ozone depletion is determined not only by heterogeneous processes on the surface of the polar stratospheric clouds, but by the gas-phase destruction as well.
Arseniy Karagodin-Doyennel, Eugene Rozanov, Ales Kuchar, William Ball, Pavle Arsenovic, Ellis Remsberg, Patrick Jöckel, Markus Kunze, David A. Plummer, Andrea Stenke, Daniel Marsh, Doug Kinnison, and Thomas Peter
Atmos. Chem. Phys., 21, 201–216, https://doi.org/10.5194/acp-21-201-2021, https://doi.org/10.5194/acp-21-201-2021, 2021
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The solar signal in the mesospheric H2O and CO was extracted from the CCMI-1 model simulations and satellite observations using multiple linear regression (MLR) analysis. MLR analysis shows a pronounced and statistically robust solar signal in both H2O and CO. The model results show a general agreement with observations reproducing a negative/positive solar signal in H2O/CO. The pattern of the solar signal varies among the considered models, reflecting some differences in the model setup.
Cited articles
Andrews, D. G. and McIntyre, M. E.: Planetary waves in horizontal and
vertical shear: The generalized Eliassen-Palm relation and the mean zonal
acceleration, J. Atmos. Sci., 33, 2031–2048,
https://doi.org/10.1175/1520-0469(1976)033<2031:PWIHAV>2.0.CO;2, 1976.
Butchart, N.: The Brewer-Dobson circulation, Rev. Geophys., 52, 157–184,
https://doi.org/10.1002/2013RG000448, 2014.
Chang, L. C., Yue, L., Wang, W., Wu, Q., and Meier, R. R.: Quasi two day
wave-related variability in the background dynamics and composition of the
mesosphere/thermosphere and the ionosphere, J. Geophys. Res.-Space, 119, 4786–4804, 2014.
Charney, J. G. and Drazin, P. G.: Propagation of planetary-scale
disturbances from the lower into the upper atmosphere, J. Geophys. Res., 66,
83–109, 1961.
Clark, R., Burrage, M., Franke, S., Manson, A., Meek, C., Mitchell, N., and
Muller, H.: Observations of 7-d planetary waves with MLT radars and the
UARS-HRDI instrument, J. Atmos. Sol.-Terr. Phy.,
64, 1217–1228, 2002.
Day, K. A., Hibbins, R. E., and Mitchell, N. J.: Aura MLS observations of the westward-propagating s=1, 16-day planetary wave in the stratosphere, mesosphere and lower thermosphere, Atmos. Chem. Phys., 11, 4149–4161, https://doi.org/10.5194/acp-11-4149-2011, 2011.
Didenko, K. A., Koval, A. V., Ermakova, T. S., and Lifar, V. D.: Interactions of stationary planetary waves during winter 2008–2009 and 2018–2019 sudden stratospheric warmings, Proc. of SPIE, 28th International Symposium on Atmospheric and Ocean Optics, Atmospheric Physics, https://doi.org/10.1117/12.2644458, 2022.
Drob, D. P., Emmert, J. T., Meriwether, J. W., Makela, J. J., Doornbos, E.,
Conde, M., Hernandez, G., Noto, G., Zawdie, K. A., McDonald, S. E., Huba, J.
D., and Klenzing, J. H.: An update to the Horizontal Wind Model (HWM): The
quiet time thermosphere, Earth and Space Science, 2, 301–319,
https://doi.org/10.1002/2014EA000089, 2015.
Eliassen A. and Palm E.: On the transfer of energy in stationary mountain
waves, Geophys. Norv., 22, 1–23, 1961.
Emmert, J. T., Drob, D. P., Picone, J. M., Siskind, D. E., Jones, M. Jr.,
Mlynczak, M. G., Bernath, P. F., Chu, X., Doornbos, E., Funke, B., Goncharenko, L. P., Hervig, M. E., Schwartz, M. J., Sheese, P. E., Vargas, F., Williams, B. P., and Yuan, T.: NRLMSIS 2.0: A whole-atmosphere empirical model of
temperature and neutral species densities, Earth and Space Science, 7,
e2020EA001321, https://doi.org/10.1029/2020EA001321, 2020.
Ermakova T. S., Aniskina, O. G., Statnaya, I. A., Motsakov, M. A., and
Pogoreltsev A. I.: Simulation of the ENSO influence on the extra-tropical
middle atmosphere, Earth Planets Space, 71, 8,
https://doi.org/10.1186/s40623-019-0987-9, 2019.
Forbes, J. M. and Zhang, X.: The quasi-6 day wave and its interactions with
solar tides, J. Geophys. Res.-Space, 122,
4764–4776, https://doi.org/10.1002/2017JA023954, 2017.
Forbes, J. M., Zhang, X., and Maute, A.: Planetary wave (PW) generation in
the thermosphere driven by the PW-modulated tidal spectrum, J.
Geophys. Res.-Space, 125, e2019JA027704,
https://doi.org/10.1029/2019JA027704, 2020.
Forbes, J. M., Zhang, X., Maute, A., and Hagan, M. E.: Zonally symmetric
oscillations of the thermosphere at planetary wave periods, J.
Geophys. Res.-Space, 123, 4110–4128,
https://doi.org/10.1002/2018JA025258, 2018.
Gavrilov, N. M. and Koval, A. V.: Parameterization of mesoscale stationary orographic wave forcing for use in numerical models of atmospheric dynamics, Izv. Atmos. Ocean. Phys., 49, 244–251 https://doi.org/10.1134/S0001433813030067, 2013.
Gavrilov, N. M., Koval, A. V., Pogoreltsev, A. I., and Savenkova, E. N.:
Simulating planetary wave propagation to the upper atmosphere during
stratospheric warming events at different mountain wave scenarios, Adv.
Space Res., 61, 1819–1836, https://doi.org/10.1016/j.asr.2017.08.022, 2018.
He, M., Chau, J. L., Forbes, J. M., Thorsen, D., Li, G., Siddiqui, T. A., Yamazaki, Y., and Hocking, W. K.: Quasi-10-day wave and semidiurnal tide nonlinear interactions during
the Southern Hemispheric SSW 2019 observed in the Northern Hemispheric
mesosphere, Geophys. Res. Lett., 47, e2020GL091453,
https://doi.org/10.1029/2020GL091453, 2020.
Holton, J. R.: The dynamic meteorology of the stratosphere and mesosphere,
Meteorol. Monogr., 15, 218, https://doi.org/10.1002/qj.49710243325, 1975.
Holton, J. R. and Tan, H.: The influence of the equatorial quasibiennial
oscillation on the global circulation at 50 mb, J. Atmos. Sci., 37,
2200–2208, 1980.
Holton, J. R., Haynes, P. H., McIntyre, M. E., Douglas, A. R., Rood, R. B.,
and Pfister, L.: Stratosphere-troposphere exchange, Rev. Geophys., 33,
403–439, 1995.
Huang, Y., Zhang, S., Li, C., Li, H., Huang, K., and Huang, C.: Annual and
interannual variations in global 6.5 DWS from 20 to 110 km during 2002–2016
observed by TIMED/SABER, J. Geophys. Res.-Space,
122, 8985–9002, https://doi.org/10.1002/2017JA023886, 2017.
Jiang, G., Xu, J., Xiong, J., Ma, R., Ning, B., Murayama, Y., Thorsen, D., Gurubaran, S., Vincent, R. A., Reid, I., and Franke, S. J.: A
case study of the mesospheric 6.5-day wave observed by radar systems,
J. Geophys. Res., 113, D16111,
https://doi.org/10.1029/2008JD009907, 2008.
Koval, A. V., Gavrilov, N. M., Pogoreltsev, A. I., and Shevchuk, N. O.:
Influence of solar activity on penetration of traveling planetary-scale waves
from the troposphere into the thermosphere, J. Geophys. Res.-Space, 123, 6888–6903, https://doi.org/10.1029/2018JA025680,
2018a.
Koval, A. V., Gavrilov, N. M., Pogoreltsev, A. I., and Savenkova, E. N.:
Comparisons of planetary wave propagation to the upper atmosphere during
stratospheric warming events at different QBO phases, J. Atmos.
Sol.-Terr. Phy., 171, 201–209,
https://doi.org/10.1016/j.jastp.2017.04.013, 2018b.
Koval, A. V., Gavrilov, N. M., Pogoreltsev, A. I., and Kandieva, K. K.:
Dynamical impacts of stratospheric QBO on the global circulation up to the
lower thermosphere, J. Geophys. Res.-Atmos., 127,
e2021JD036095, https://doi.org/10.1029/2021JD036095, 2022a.
Koval, A. V., Gavrilov, N. M., Kandieva, K. K. Ermakova, T. S., and Didenko, K. A.:
Numerical simulation of stratospheric QBO impact on the planetary waves up
to the thermosphere, Sci. Rep., 12, 21701, https://doi.org/10.1038/s41598-022-26311-x 2022b.
Lindzen, R. S.: Turbulence and stress owing to gravity wave and tidal breakdown, J. Geophys. Res., 86, 9707–9714, 1981.
Liu, H. L., Talaat, E. R., Roble, R. G., Lieberman, R. S., Riggin D. M., and
Yee, J. H.: The 6.5-day wave and its seasonal variability in the middle and
upper atmosphere, J. Geophy. Res.-Atmos., 109, D21112,
https://doi.org/10.1029/2004jd004795, 2004.
Longuet-Higgins, M. S.: The eigenfunctions of Laplace's tidal equation over
a sphere, Philos. T. R. Soc. Lond., 262, 511–607, 1968.
Matsuno, T.: Vertical propagation of stationary planetary waves in the winter
Northern Hemisphere, J. Atmos. Sci., 27, 871–883, 1970.
Medvedeva, I. V., Semenov, A. I., Pogoreltsev, A. I., and Tatarnikov, A. V.:
Influence of sudden stratospheric warming on the mesosphere/lower
thermosphere from the hydroxyl emission observations and numerical
simulations, J. Atmos. Sol.-Terr. Phy., 187,
22–32, https://doi.org/10.1016/j.jastp.2019.02.005, 2019.
Merzlyakov, E., Solovjova, T., and Yudakov, A.: The interannual variability
of a 5–7 day wave in the middle atmosphere in autumn from era product data,
aura MLS data, and meteor wind data, J. Atmos.
Sol.-Terr. Phy., 102, 281–289, 2013.
Nath, D., Chen, W., Zelin, C., Pogoreltsev, A. I., and Wei, K. Dynamics of
2013 Sudden Stratospheric Warming event and its impact on cold weather over
Eurasia: Role of planetary wave reflection, Sci. Rep., 6, 24174,
https://doi.org/10.1038/srep24174, 2016.
Newman, P. A., Oman, L. D., Douglass, A. R., Fleming, E. L., Frith, S. M., Hurwitz, M. M., Kawa, S. R., Jackman, C. H., Krotkov, N. A., Nash, E. R., Nielsen, J. E., Pawson, S., Stolarski, R. S., and Velders, G. J. M.: What would have happened to the ozone layer if chlorofluorocarbons (CFCs) had not been regulated?, Atmos. Chem. Phys., 9, 2113–2128, https://doi.org/10.5194/acp-9-2113-2009, 2009.
Pancheva, D., Mukhtarov, P., Andonov, B., Mitchell, N. J., and Forbes, J. M.
Planetary waves observed by TIMED/SABER in coupling the stratosphere-
mesosphere-lower thermosphere during the winter of 2003/2004: part
2 – altitude and latitude planetary wave structure, J. Atmos. Sol.-Terr.
Phy., 71, 75–87, https://doi.org/10.1016/j.jastp.2008.09.027, 2009.
Pancheva, D., Mukhtarov, P., Andonov, B., and Forbes, J. M.: Global
distribution and climatological features of the 5–6-day planetary waves seen
in the SABER/TIMED temperatures (2002–2007), J. Atmos. Sol.-Terr. Phy., 72,
26–37, 2010.
Pancheva, D., Mukhtarov, P., and Siskind, D. E.: The quasi-6-day waves in
NOGAPS-ALPHA forecast model and their climatology in MLS/Aura measurements
(2005–2014), J. Atmos. Sol.-Terr. Phy., 181,
19–37, 2018.
Pedatella, N. M. and Forbes, J. M.: Modulation of the equatorial F-region by
the quasi-16-day planetary wave, Geophys. Res. Lett., 36, L09105,
https://doi.org/10.1029/2009GL037809, 2009.
Pogoreltsev, A. I.: Simulation of planetary waves and their influence on the
zonally averaged circulation in the middle atmosphere, Earth Planets Space,
51, 773–784, 1999.
Pogoreltsev,
A. I.: Numerical simulation of secondary planetary waves arising
from the nonlinear interaction of the normal atmospheric modes, Phys. Chem.
Earth Pt. C, 26, 395–403, 2001.
Pogoreltsev, A. I.: Generation of normal atmospheric modes by
stratospheric vacillations, Izv. Atmos. Ocean. Phy., 43, 423–435, 2007.
Pogoreltsev, A. I., Vlasov, A. A., Froehlich, K., and Jacobi, Ch.: Planetary
waves in coupling the lower and upper atmosphere, J. Atmos. Sol.-Terr.
Phy., 69, 2083–2101, https://doi.org/10.1016/j.jastp.2007.05.014, 2007.
Pogoreltsev, A. I., Savenkova, E. N., and Pertsev, N. N.: Sudden stratopheric
warmings: the role of normal atmospheric modes, Geomagn. Aeronomy,
54, 1–15, doi 10.1134/S0016793214020169, 2014.
Qin, Y., Gu, S.-Y., and Dou, X.: A new mechanism for the generation of
quasi-6-day and quasi-10-day waves during the 2019 Antarctic sudden
stratospheric warming, J. Geophys. Res.-Atmos., 126,
e2021JD035568, https://doi.org/10.1029/2021JD035568, 2021.
Sassi, F., Garcia, R., and Hoppel, K.: Large-scale Rossby normal modes
during some recent Northern Hemisphere winters, J. Atmos.
Sci., 69, 820–839, 2012.
Schoeberl, M.: Stratospheric warmings – observations and theory, Rev.
Geophys., 16, 521–538, https://doi.org/10.1029/RG016i004p00521, 1978.
Shevchuk N. O., Ortikov, M. Yu., and Pogoreltsev, A. I.: Modeling of atmospheric
tides with account of diurnal variations of ionospheric conductivity,
Russ. J. Phys. Chem. B, 12, 576–589, https://doi.org/10.1134/S199079311803017X, 2018.
Suvorova, E. V. and Pogoreltsev, A. I.: Modeling of nonmigrating tides in the
middle atmosphere, Geomagmetizm and Aeronomy, 51, 105–115, https://doi.org/10.1134/S0016793210061039, 2011.
Swarztrauber, P. N. and Kasahara, A.: The vector harmonic analysis of
Laplace's tidal equations, SIAM J. Sci. Stat. Comp., 6, 464–491, 1985.
Wang, J. C., Chang, L. C., Yue, J., Wang, W., and Siskind, D. E.: The quasi
2 day wave response in TIME-GCM nudged with NOGAPS-ALPHA, J.
Geophys. Res.-Space, 122, 5709–5732, 2017.
Yamazaki, Y., Matthias, V., and Miyoshi, Y.: Quasi-4-day wave: Atmospheric
manifestation of the first symmetric Rossby normal mode of zonal wavenumber
2, J. Geophys. Res.-Atmos., 126, e2021JD034855,
https://doi.org/10.1029/2021JD034855, 2021.
Yiğit, E., and Medvedev, A. S.: Heating and cooling of the thermo-sphere by internal gravity waves, Geophys. Res. Lett., 36, L14807, https://doi.org/10.1029/2009GL038507, 2009.
Short summary
Periodic changes in all hydrodynamic parameters are constantly observed in the atmosphere. The amplitude of these fluctuations increases with height due to a decrease in the atmospheric density. In the upper layers of the atmosphere, waves are the dominant form of motion. We use a model of the general circulation of the atmosphere to study the contribution to the formation of the dynamic and temperature regimes of the middle and upper atmosphere made by different global-scale atmospheric waves.
Periodic changes in all hydrodynamic parameters are constantly observed in the atmosphere. The...
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