Links between Solar Activity and Atmospheric Circulation (2nd Volume)

A special issue of Atmosphere (ISSN 2073-4433). This special issue belongs to the section "Upper Atmosphere".

Deadline for manuscript submissions: closed (15 July 2022) | Viewed by 1991

Special Issue Editors


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Guest Editor
Central Aerological Observatory, Dolgoprudny, Pervomayskaya Str. 3, Russia
Interests: solar activity; solar-terrestrial connections; global models; atmospheric circulation

E-Mail Website
Guest Editor
Central Aerological Observatory, Dolgoprudny, Pervomayskaya Str. 3, Russia
Interests: middle atmosphere; global models; solar cycle; solar proton events

Special Issue Information

Dear Colleagues,

The influence of solar activity and associated disturbances of interplanetary medium on the middle atmosphere circulation remains the most important problem in solar-terrestrial physics. The middle atmospher (stratosphere, mesosphere and lower thermosphere, which cover 10-100 km range of altitudes ) is the region of intensive interaction between dynamics and chemical composition. The primary constituents in the lower and middle atmosphere are diatomic nitrogen and oxygen, which together account for 98.65 % of the total mass of the dry atmosphere. The primary constituents have no significant sources or sinks in the stratosphere or mesosphere, so that their mass fractions are nearly constant in height. Solar UV radiation between 100 and 300 nm dissociates primary constituents and that gives the start to many chemical reactions, for example, the reaction of ozone prduction. The important role of oxygen and ozone in the middle atmosphere is heating, which generates the temperature structure of the atmosphere between tropopouse and thermopouse.

Temperature fields and wind fields are closely connected by fundamental equations (A simple example is geostrophic approximation). Therefore, solar UV radiation strongly controls chemistry and dynamics, and its observed variability (solar cycle) leads to correspondents in temperature, winds and composition. Another factor that may disturb polar ozone (and then dynamics) in polar regions is solar energetic particles, which penetrate to the middle atmosphere during solar proton events.

Therefore, such a complicated situation needs detailed knowledge about observed satellite UV measurements, solar particles and corresponded ionization caused in both polar regions, numerical models, which may calculate circulation in the presence of all mentioned above factors, which are the focus of this Special Issue.

Dr. Alexei Krivolutsky
Dr. Anna Kukoleva
Guest Editors

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Keywords

  • solar forcing
  • solar–atmospheric links
  • atmospheric circulation
  • global models

Published Papers (1 paper)

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Research

10 pages, 2053 KiB  
Article
Sensitivity of the 4–10-Day Planetary Wave Structures in the Middle Atmosphere to the Solar Activity Effects in the Thermosphere
by Andrey V. Koval, Nikolai M. Gavrilov, Ksenia A. Didenko, Tatiana S. Ermakova and Elena N. Savenkova
Atmosphere 2022, 13(8), 1325; https://doi.org/10.3390/atmos13081325 - 19 Aug 2022
Cited by 3 | Viewed by 1663
Abstract
Numerical simulation of the general atmospheric circulation was performed to estimate changes in amplitudes of the westward-travelling planetary waves (PWs) at altitudes from the Earth’s surface up to 300 km under different solar activity (SA) levels. The three-dimensional nonlinear mechanistic model of circulation [...] Read more.
Numerical simulation of the general atmospheric circulation was performed to estimate changes in amplitudes of the westward-travelling planetary waves (PWs) at altitudes from the Earth’s surface up to 300 km under different solar activity (SA) levels. The three-dimensional nonlinear mechanistic model of circulation of the middle and upper atmosphere “MUAM” was used. The atmospheric general circulation and PW amplitudes were calculated based on ensembles containing 16 model runs for conditions corresponding to low and high SA. PWs having periods of 4–10 days were considered. Comparison with the data of digital ionosondes showed that the MUAM model is capable of reproducing the considered PW modes at thermospheric heights. It is shown that under high SA conditions, PW amplitudes are significantly larger in the thermosphere and smaller in the middle atmosphere. The observed PW structures are influenced not only by changes in atmospheric refractive index and Eliassen–Palm flux but also by varying PW reflection in the lower thermosphere, which can change proportions of the wave energy transferred from the lower atmosphere to the upper layers and reflected downwards. Full article
(This article belongs to the Special Issue Links between Solar Activity and Atmospheric Circulation (2nd Volume))
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