Solar-Terrestrial Physics Solar-Terrestrial Physics Solar-Terrestrial Physics 2500-0535 24518 10.12737/stp-44201807 Results of current research Results of current research Results of current research Changes in the middle and upper atmosphere parameters during the January 2013 sudden stratospheric warming Changes in the middle and upper atmosphere parameters during the January 2013 sudden stratospheric warming Ясюкевич Анна Сергеевна Yasyukevich Anna Sergeevna annpol@iszf.irk.ru

кандидат физико-математических наук;

candidate of physical and mathematical sciences;

 Клименко Максим Владимирович Klimenko Maksim Vladimirovich maksim.klimenko@mail.ru

кандидат физико-математических наук;

candidate of physical and mathematical sciences;

 Куликов Юрий Юрьевич Kulikov Yury Yuryevich yuyukul@appl.sci-nnov.ru Клименко Владимир Викторович Klimenko Vladimir Viktorovich vvk_48@mail.ru

кандидат физико-математических наук;

candidate of physical and mathematical sciences;

 Бессараб Федор Семенович Bessarab Fedor Semenovich FBESSARAB@kantiana.ru

кандидат физико-математических наук;

candidate of physical and mathematical sciences;

 Кореньков Юрий Николаевич Korenkov Yuriy Nikolaevich kor_yu@mail.ru

доктор физико-математических наук;

doctor of physical and mathematical sciences;

 Маричев Валерий Николаевич Marichev Valery Nikolaevich marichev@iao.ru

доктор физико-математических наук;

doctor of physical and mathematical sciences;

 https://orcid.org/0000-0002-0847-3553 Ратовский Константин Геннадьевич Ratovsky Konstantin Gennadyevich ratovsky@iszf.irk.ru

кандидат физико-математических наук;

candidate of physical and mathematical sciences;

 Колесник Сергей Анатольевич Kolesnik Sergey Anatol'evich serkol@mail.tsu.ru Институт солнечно-земной физики СО РАН Иркутск Россия Institute of Solar Terrestrial Physics SB RAS Irkutsk Russian Federation Западное отделение ИЗМИРАН Калининград Россия WD IZMIRAN Kaliningrad Russian Federation Балтийский федеральный университет имени И. Канта Калининград Россия I. Kant Baltic Federal University Kaliningrad Russian Federation Институт прикладной физики РАН Нижний Новгород Россия Institute of Applied Physics RAS Nizhny Novgorod Russian Federation Западное отделение ИЗМИРАН Калининград Россия WD IZMIRAN Kaliningrad Russian Federation Калининградский филиал Института земного магнетизма, ионосферы и распространения радиоволн им. Н.В. Пушкова РАН Калининград Россия West Department of Pushkov Institute of Terrestrial Mag-netism, Ionosphere and Radio Wave Propagation RAS Kaliningrad Russian Federation Балтийский федеральный университет имени И. Канта Калининград Россия I. Kant Baltic Federal University Kaliningrad Russian Federation Западное отделение ИЗМИРАН Калининград Россия WD IZMIRAN Kaliningrad Russian Federation Институт оптики атмосферы им. В.Е. Зуева СО РАН Томск Россия V.E. Zuev Institute of Atmospheric Optics SB RAS Tomsk Russian Federation Институт солнечно-земной физики СО РАН Иркутск Россия Institute of Solar-Terrestrial Physics SB RAS Irkutsk Russian Federation Томский государственный университет Tomsk State University 4 4 48 58 https://zh-szf.ru/en/nauka/article/24518/view

We present the results of complex obser-vations of various parameters of the middle and upper atmosphere over Siberia in December 2012 – January 2013, during a major sudden stratospheric warming (SSW) event. We analyze variations in ozone concentration from microwave measurements, in stratosphere and lower mesosphere temperatures from lidar and satellite measurements, in the F2-layer critical frequency (foF2), in the total electron content (TEC), as well as in the ratio of concentrations of atomic oxygen to molecular nitrogen (O/N2) in the thermosphere. To interpret the observed disturbances in the upper atmosphere, the experimental measurements are compared with the results of model calculations obtained with the Global Self-consistent Model of Thermosphere—Ionosphere—Protonosphere (GSM TIP). The response of the upper atmosphere to the SSW event is shown to be a decrease in foF2 and TEC during the evolution of the warming event and a prolonged increase in O/N2, foF2, and TEC after the SSW maximum. For the first time, we observe the relation between the increase in stratospheric ozone, thermospheric O/N2, and ionospheric electron density for a fairly long time (up to 20 days) after the SSW maximum at midlatitudes.

We present the results of complex obser-vations of various parameters of the middle and upper atmosphere over Siberia in December 2012 – January 2013, during a major sudden stratospheric warming (SSW) event. We analyze variations in ozone concentration from microwave measurements, in stratosphere and lower mesosphere temperatures from lidar and satellite measurements, in the F2-layer critical frequency (foF2), in the total electron content (TEC), as well as in the ratio of concentrations of atomic oxygen to molecular nitrogen (O/N2) in the thermosphere. To interpret the observed disturbances in the upper atmosphere, the experimental measurements are compared with the results of model calculations obtained with the Global Self-consistent Model of Thermosphere—Ionosphere—Protonosphere (GSM TIP). The response of the upper atmosphere to the SSW event is shown to be a decrease in foF2 and TEC during the evolution of the warming event and a prolonged increase in O/N2, foF2, and TEC after the SSW maximum. For the first time, we observe the relation between the increase in stratospheric ozone, thermospheric O/N2, and ionospheric electron density for a fairly long time (up to 20 days) after the SSW maximum at midlatitudes.

 sudden stratospheric warming ozone stratosphere ionosphere electron density total electron content atmosphere-ionosphere coupling sudden stratospheric warming ozone stratosphere ionosphere electron density total electron content atmosphere-ionosphere coupling

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