Numerical Modeling of the Influence of Solar Activity on the Global Circulation in the Earth’s Mesosphere and Lower Thermosphere
The nonhydrostatic model of the global neutral wind system of the earth’s atmosphere, developed earlier in the Polar Geophysical Institute, is utilized to investigate how solar activity affects the formation of the large-scale global circulation of the mesosphere and lower thermosphere. The peculiar...
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Series: | International Journal of Geophysics |
Online Access: | http://dx.doi.org/10.1155/2012/106035 |
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doaj-19f34d41ba4949a68593bf235e36b7ee2020-11-24T23:46:59ZengHindawi LimitedInternational Journal of Geophysics1687-885X1687-88682012-01-01201210.1155/2012/106035106035Numerical Modeling of the Influence of Solar Activity on the Global Circulation in the Earth’s Mesosphere and Lower ThermosphereIgor Mingalev0Victor Mingalev1Kola Scientific Center of the Russian Academy of Sciences, Polar Geophysical Institute, Fersman Street 14, Apatity 184209, RussiaKola Scientific Center of the Russian Academy of Sciences, Polar Geophysical Institute, Fersman Street 14, Apatity 184209, RussiaThe nonhydrostatic model of the global neutral wind system of the earth’s atmosphere, developed earlier in the Polar Geophysical Institute, is utilized to investigate how solar activity affects the formation of the large-scale global circulation of the mesosphere and lower thermosphere. The peculiarity of the utilized model consists in that the internal energy equation for the neutral gas is not solved in the model calculations. Instead, the global temperature field is assumed to be a given distribution, that is, the input parameter of the model. Moreover, in the model calculations, not only the horizontal components but also the vertical component of the neutral wind velocity is obtained by means of a numerical solution of a generalized Navier-Stokes equation for compressible gas, so the hydrostatic equation is not applied. The simulation results indicate that solar activity ought to influence considerably on the formation of global neutral wind system in the mesosphere and lower thermosphere. The influence is conditioned by the vertical transport of air from the lower thermosphere to the mesosphere and stratosphere. This transport may be rather different under distinct solar activity conditions.http://dx.doi.org/10.1155/2012/106035 |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Igor Mingalev Victor Mingalev |
spellingShingle |
Igor Mingalev Victor Mingalev Numerical Modeling of the Influence of Solar Activity on the Global Circulation in the Earth’s Mesosphere and Lower Thermosphere International Journal of Geophysics |
author_facet |
Igor Mingalev Victor Mingalev |
author_sort |
Igor Mingalev |
title |
Numerical Modeling of the Influence of Solar Activity on the Global Circulation in the Earth’s Mesosphere and Lower Thermosphere |
title_short |
Numerical Modeling of the Influence of Solar Activity on the Global Circulation in the Earth’s Mesosphere and Lower Thermosphere |
title_full |
Numerical Modeling of the Influence of Solar Activity on the Global Circulation in the Earth’s Mesosphere and Lower Thermosphere |
title_fullStr |
Numerical Modeling of the Influence of Solar Activity on the Global Circulation in the Earth’s Mesosphere and Lower Thermosphere |
title_full_unstemmed |
Numerical Modeling of the Influence of Solar Activity on the Global Circulation in the Earth’s Mesosphere and Lower Thermosphere |
title_sort |
numerical modeling of the influence of solar activity on the global circulation in the earth’s mesosphere and lower thermosphere |
publisher |
Hindawi Limited |
series |
International Journal of Geophysics |
issn |
1687-885X 1687-8868 |
publishDate |
2012-01-01 |
description |
The nonhydrostatic model of the global neutral wind system of the earth’s atmosphere, developed earlier in the Polar Geophysical Institute, is utilized to investigate how solar activity affects the formation of the large-scale global circulation of the mesosphere and lower thermosphere. The peculiarity of the utilized model consists in that the internal energy equation for the neutral gas is not solved in the model calculations. Instead, the global temperature field is assumed to be a given distribution, that is, the input parameter of the model. Moreover, in the model calculations, not only the horizontal components but also the vertical component of the neutral wind velocity is obtained by means of a numerical solution of a generalized Navier-Stokes equation for compressible gas, so the hydrostatic equation is not applied. The simulation results indicate that solar activity ought to influence considerably on the formation of global neutral wind system in the mesosphere and lower thermosphere. The influence is conditioned by the vertical transport of air from the lower thermosphere to the mesosphere and stratosphere. This transport may be rather different under distinct solar activity conditions. |
url |
http://dx.doi.org/10.1155/2012/106035 |
work_keys_str_mv |
AT igormingalev numericalmodelingoftheinfluenceofsolaractivityontheglobalcirculationintheearthsmesosphereandlowerthermosphere AT victormingalev numericalmodelingoftheinfluenceofsolaractivityontheglobalcirculationintheearthsmesosphereandlowerthermosphere |
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