Modeling of the effect of internal gravity waves on upper atmospheric conditions during sudden stratospheric warming

We present results of modeling of the effect of internal gravity waves (IGW), excited in the region of development of a sudden stratospheric warming (SSW), on upper atmospheric conditions. In the numerical experiment, we use a two-dimensional model of propagation of atmospheric waves, taking into ac...

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Main Authors: Vasilyev P.A., Karpov I.V., Kshevetskii S.P.
Format: Article
Language:English
Published: INFRA-M 2016-09-01
Series:Solar-Terrestrial Physics
Subjects:
Online Access:https://naukaru.ru/ru/nauka/article/13708/view
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spelling doaj-0d6101f228734667a93ea40bc5fa6fa42020-11-25T00:32:46ZengINFRA-M Solar-Terrestrial Physics2500-05352016-09-01239910510.12737/22288Modeling of the effect of internal gravity waves on upper atmospheric conditions during sudden stratospheric warmingVasilyev P.A.0Karpov I.V.1Kshevetskii S.P.2I. Kant Baltic Federal University, Kaliningrad, RussiaI. Kant Baltic Federal University, Kaliningrad, Russia; WD IZMIRAN, Kaliningrad, RussiaI. Kant Baltic Federal University, Kaliningrad, Russia We present results of modeling of the effect of internal gravity waves (IGW), excited in the region of development of a sudden stratospheric warming (SSW), on upper atmospheric conditions. In the numerical experiment, we use a two-dimensional model of propagation of atmospheric waves, taking into account dissipative and nonlinear processes accompanying wave propagation. As a source of disturbances we consider temperature and density disturbances in the stratosphere during SSWs. Amplitude and frequency characteristics of the source of disturbances are estimated from observations and IGW theory. Numerical calculations showed that waves generated at stratospheric heights during SSW can cause temperature changes in the upper atmosphere. Maximum relative disturbances, caused by such waves, with respect to quiet conditions are observed at 100–200 km. Disturbances of the upper atmosphere in turn have an effect on the dynamics of charged component in the ionosphere and can contribute to observable ionospheric effects of SSW.https://naukaru.ru/ru/nauka/article/13708/viewInternal gravity wavessudden stratospheric warmingsmodeling
collection DOAJ
language English
format Article
sources DOAJ
author Vasilyev P.A.
Karpov I.V.
Kshevetskii S.P.
spellingShingle Vasilyev P.A.
Karpov I.V.
Kshevetskii S.P.
Modeling of the effect of internal gravity waves on upper atmospheric conditions during sudden stratospheric warming
Solar-Terrestrial Physics
Internal gravity waves
sudden stratospheric warmings
modeling
author_facet Vasilyev P.A.
Karpov I.V.
Kshevetskii S.P.
author_sort Vasilyev P.A.
title Modeling of the effect of internal gravity waves on upper atmospheric conditions during sudden stratospheric warming
title_short Modeling of the effect of internal gravity waves on upper atmospheric conditions during sudden stratospheric warming
title_full Modeling of the effect of internal gravity waves on upper atmospheric conditions during sudden stratospheric warming
title_fullStr Modeling of the effect of internal gravity waves on upper atmospheric conditions during sudden stratospheric warming
title_full_unstemmed Modeling of the effect of internal gravity waves on upper atmospheric conditions during sudden stratospheric warming
title_sort modeling of the effect of internal gravity waves on upper atmospheric conditions during sudden stratospheric warming
publisher INFRA-M
series Solar-Terrestrial Physics
issn 2500-0535
publishDate 2016-09-01
description We present results of modeling of the effect of internal gravity waves (IGW), excited in the region of development of a sudden stratospheric warming (SSW), on upper atmospheric conditions. In the numerical experiment, we use a two-dimensional model of propagation of atmospheric waves, taking into account dissipative and nonlinear processes accompanying wave propagation. As a source of disturbances we consider temperature and density disturbances in the stratosphere during SSWs. Amplitude and frequency characteristics of the source of disturbances are estimated from observations and IGW theory. Numerical calculations showed that waves generated at stratospheric heights during SSW can cause temperature changes in the upper atmosphere. Maximum relative disturbances, caused by such waves, with respect to quiet conditions are observed at 100–200 km. Disturbances of the upper atmosphere in turn have an effect on the dynamics of charged component in the ionosphere and can contribute to observable ionospheric effects of SSW.
topic Internal gravity waves
sudden stratospheric warmings
modeling
url https://naukaru.ru/ru/nauka/article/13708/view
work_keys_str_mv AT vasilyevpa modelingoftheeffectofinternalgravitywavesonupperatmosphericconditionsduringsuddenstratosphericwarming
AT karpoviv modelingoftheeffectofinternalgravitywavesonupperatmosphericconditionsduringsuddenstratosphericwarming
AT kshevetskiisp modelingoftheeffectofinternalgravitywavesonupperatmosphericconditionsduringsuddenstratosphericwarming
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