Modeling the impact of solar activity variations on global atmospheric circulation
In this study, we continue a series of works devoted to modeling and studying the sensitivity of global atmospheric dynamic processes to variations in solar emissions during the 11-year solar activity (SA) cycle. We focus on studying the response of meridional atmospheric circulation in the middle a...
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Published in | Solar-terrestrial physics Vol. 10; no. 2; pp. 111 - 118 |
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Main Authors | , , , , |
Format | Journal Article |
Language | English |
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25.06.2024
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Abstract | In this study, we continue a series of works devoted to modeling and studying the sensitivity of global atmospheric dynamic processes to variations in solar emissions during the 11-year solar activity (SA) cycle. We focus on studying the response of meridional atmospheric circulation in the middle atmosphere to changes in thermosphere characteristics with changes in SA. For this purpose, numerical simulations of the general atmospheric circulation were carried out using the nonlinear numerical circulation model of the middle and upper atmosphere MUAM. The main mechanism of the influence of thermospheric disturbances on the underlying layers is assumed to be a change in the conditions of propagation and reflection of planetary waves (PWs) due to changes in SA. Changes in temperature, zonal and meridional wind are shown to localize along waveguides, demonstrating the significant role of PWs in transmitting thermospheric disturbances, caused by changes in SA, to the middle atmosphere. The magnitude of changes in meridional circulation can reach 10 % in the northern stratosphere between SA maxima and minima. |
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AbstractList | In this study, we continue a series of works devoted to modeling and studying the sensitivity of global atmospheric dynamic processes to variations in solar emissions during the 11-year solar activity (SA) cycle. We focus on studying the response of meridional atmospheric circulation in the middle atmosphere to changes in thermosphere characteristics with changes in SA. For this purpose, numerical simulations of the general atmospheric circulation were carried out using the nonlinear numerical circulation model of the middle and upper atmosphere MUAM. The main mechanism of the influence of thermospheric disturbances on the underlying layers is assumed to be a change in the conditions of propagation and reflection of planetary waves (PWs) due to changes in SA. Changes in temperature, zonal and meridional wind are shown to localize along waveguides, demonstrating the significant role of PWs in transmitting thermospheric disturbances, caused by changes in SA, to the middle atmosphere. The magnitude of changes in meridional circulation can reach 10 % in the northern stratosphere between SA maxima and minima. |
Author | Didenko, Kseniia Koval, Andrey Ermakova, Tatiana Golovko, Anastasiya Gavrilov, Nikolay |
Author_xml | – sequence: 1 givenname: Andrey surname: Koval fullname: Koval, Andrey organization: Saint Petersburg State University – sequence: 2 givenname: Nikolay surname: Gavrilov fullname: Gavrilov, Nikolay organization: Saint-Petersburg State University – sequence: 3 givenname: Anastasiya surname: Golovko fullname: Golovko, Anastasiya organization: St. Petersburg University – sequence: 4 givenname: Kseniia surname: Didenko fullname: Didenko, Kseniia organization: Pushkov Institute of Terrestrial Magnetism, Ionosphere, and Radio Wave Propagation RAS, St. Petersburg University – sequence: 5 givenname: Tatiana surname: Ermakova fullname: Ermakova, Tatiana organization: Russian State Hydrometeorological University, St. Petersburg University |
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Cites_doi | 10.1175/BAMS-86-8-1117 10.1186/s40623-015-0259-2 10.1175/JCLI-D-17-0202.1 10.1002/2014JA019936 10.1029/2008JA013448 10.1002/qj.49707532603 10.1134/S0016793215060067 10.1127/0941-2948/2006/0136 10.1007/s00585-997-0069-3 10.1029/2019JA027704 10.3390/atmos13081325 10.1002/2017MS001232 10.1002/2018JA025258 10.1002/2016JA023564 10.1002/2013RG000448 10.1007/lrsp-2010-1 10.12737/stp-54201907 10.1029/94JA00518 10.2151/jmsj.2015-001 10.1016/j.jastp.2007.05.014 10.1029/2008GL034575 10.1002/asl.1020 10.1029/2019JA027392 10.1256/smsqj.56811 10.1098/rspa.1956.0127 10.1002/2016JA023745 10.1029/2005JA011510 10.1007/s12040-018-0972-x 10.5194/acp-23-4105-2023 10.1029/95RG02097 10.1175/JCLI-D-16-0400.1 10.1029/JD092iD01p00829 10.1175/1520-0469(1991)048<0651:OTCOED>2.0.CO;2 10.1029/2020EA001321 10.1029/2002JD002224 10.1175/1520-0469(1980)037<1197:PWCBTT>2.0.CO;2 10.1029/2018JA025680 10.1175/BAMS-D-11-00145.1 |
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