Influence of cosmic weather on the Earth’s atmosphere

The review generalizes experimental data on the relationships between the solar activity agents (space weather) and atmosphere constituents. It is shown that high-energy solar protons (SPE) make a powerful impact on photo-chemical processes in the polar areas and, correspondingly, on atmospheric cir...

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Published in:Arctic and Antarctic Research
Main Authors: O. A. Troshichev, I. P. Gabis, A. A. Krivolutsky, О. А. Трошичев, И. П. Габис, А. А. Криволуцкий
Format: Article in Journal/Newspaper
Language:English
Published: Государственный научный центр Российской Федерации Арктический и антарктический научно-исследовательский институт 2021
Subjects:
южная осцилляция (ENSO)
Earth’s atmosphere
geoeffective solar wind
high-energy solar protons (SPE)
model computations
ozone depletion
planetary cloudiness
quasi-biennial oscillation (QBO)
solar UV irradiance
Southern Oscillation (ENSO)
Space weather
атмосферная циркуляция
высокоэнергичные солнечные протоны
геоэффективный солнечный ветер
квазидвухлетняя осцилляция (QBO)
космическая погода
модельные расчеты
озоновая «дыра»
планетарная облачность
солнечное УФ-излучение
Antarctic
The Antarctic
Antarc*
Arctic
Online Access:https://www.aaresearch.science/jour/article/view/354
https://doi.org/10.30758/0555-2648-2021-67-2-177-207
id ftjaaresearch:oai:oai.aari.elpub.ru:article/354
record_format openpolar
institution Open Polar
collection Arctic and Antarctic Research
op_collection_id ftjaaresearch
language English
topic южная осцилляция (ENSO)
Earth’s atmosphere
geoeffective solar wind
high-energy solar protons (SPE)
model computations
ozone depletion
planetary cloudiness
quasi-biennial oscillation (QBO)
solar UV irradiance
Southern Oscillation (ENSO)
Space weather
атмосферная циркуляция
высокоэнергичные солнечные протоны
геоэффективный солнечный ветер
квазидвухлетняя осцилляция (QBO)
космическая погода
модельные расчеты
озоновая «дыра»
планетарная облачность
солнечное УФ-излучение
spellingShingle южная осцилляция (ENSO)
Earth’s atmosphere
geoeffective solar wind
high-energy solar protons (SPE)
model computations
ozone depletion
planetary cloudiness
quasi-biennial oscillation (QBO)
solar UV irradiance
Southern Oscillation (ENSO)
Space weather
атмосферная циркуляция
высокоэнергичные солнечные протоны
геоэффективный солнечный ветер
квазидвухлетняя осцилляция (QBO)
космическая погода
модельные расчеты
озоновая «дыра»
планетарная облачность
солнечное УФ-излучение
O. A. Troshichev
I. P. Gabis
A. A. Krivolutsky
О. А. Трошичев
И. П. Габис
А. А. Криволуцкий
Influence of cosmic weather on the Earth’s atmosphere
topic_facet южная осцилляция (ENSO)
Earth’s atmosphere
geoeffective solar wind
high-energy solar protons (SPE)
model computations
ozone depletion
planetary cloudiness
quasi-biennial oscillation (QBO)
solar UV irradiance
Southern Oscillation (ENSO)
Space weather
атмосферная циркуляция
высокоэнергичные солнечные протоны
геоэффективный солнечный ветер
квазидвухлетняя осцилляция (QBO)
космическая погода
модельные расчеты
озоновая «дыра»
планетарная облачность
солнечное УФ-излучение
description The review generalizes experimental data on the relationships between the solar activity agents (space weather) and atmosphere constituents. It is shown that high-energy solar protons (SPE) make a powerful impact on photo-chemical processes in the polar areas and, correspondingly, on atmospheric circulation and planetary cloudiness. Variations of the solar UV irradiance modulate the descent rate of the zonal wind in the equatorial stratosphere in the course of quasi-biennial oscillation (QBO), and thus control the total duration (period) of the QBO cycle and, correspondingly, the seasonal ozone depletion in the Antarctic. The geo-effective solar wind impacts on the atmospheric wind system in the entire Southern Polar region, and influences the dynamics of the Southern Oscillation (ENSO). В обзоре обобщены экспериментальные данные о влиянии космической погоды на земную атмосферу. Показано, что высокоэнергичные солнечные протоны (SPE) оказывают мощное воздействие на фотохимические процессы в полярных областях и, соответственно, на атмосферную циркуляцию и планетарную облачность. Вариации солнечного УФ-излучения моделируют скорость спуска зональных ветров в экваториальной стратосфере в ходе квазидвухлетней осцилляции (QBO) и контролируют, таким образом, общую продолжительность (период) QBO цикла и, соответственно, вариации общего содержания озона в Антарктике. Геоэффективный солнечный ветер воздействует на систему катабатических ветров во всей южной полярной области и влияет на динамику южной осцилляции (ENSO).
format Article in Journal/Newspaper
author O. A. Troshichev
I. P. Gabis
A. A. Krivolutsky
О. А. Трошичев
И. П. Габис
А. А. Криволуцкий
author_facet O. A. Troshichev
I. P. Gabis
A. A. Krivolutsky
О. А. Трошичев
И. П. Габис
А. А. Криволуцкий
author_sort O. A. Troshichev
title Influence of cosmic weather on the Earth’s atmosphere
title_short Influence of cosmic weather on the Earth’s atmosphere
title_full Influence of cosmic weather on the Earth’s atmosphere
title_fullStr Influence of cosmic weather on the Earth’s atmosphere
title_full_unstemmed Influence of cosmic weather on the Earth’s atmosphere
title_sort influence of cosmic weather on the earth’s atmosphere
publisher Государственный научный центр Российской Федерации Арктический и антарктический научно-исследовательский институт
publishDate 2021
url https://www.aaresearch.science/jour/article/view/354
https://doi.org/10.30758/0555-2648-2021-67-2-177-207
geographic Antarctic
The Antarctic
geographic_facet Antarctic
The Antarctic
genre Antarc*
Antarctic
Arctic
genre_facet Antarc*
Antarctic
Arctic
op_source Arctic and Antarctic Research; Том 67, № 2 (2021); 177-207
Проблемы Арктики и Антарктики; Том 67, № 2 (2021); 177-207
2618-6713
0555-2648
10.30758/0555-2648-2021-67-2
op_relation https://www.aaresearch.science/jour/article/view/354/202
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spelling ftjaaresearch:oai:oai.aari.elpub.ru:article/354 2024-06-23T07:46:31+00:00 Influence of cosmic weather on the Earth’s atmosphere Влияние космической погоды на земную атмосферу O. A. Troshichev I. P. Gabis A. A. Krivolutsky О. А. Трошичев И. П. Габис А. А. Криволуцкий 2021-07-09 application/pdf https://www.aaresearch.science/jour/article/view/354 https://doi.org/10.30758/0555-2648-2021-67-2-177-207 eng eng Государственный научный центр Российской Федерации Арктический и антарктический научно-исследовательский институт https://www.aaresearch.science/jour/article/view/354/202 Thompson D.W.J., Wallace J.M. The Arctic Oscillation signature in the wintertime geopotential height and temperature fields. Geophys. Res. Let. 1998, 25 (9): 1297–1300. Philander S.G.H., Rasmusson E.M. The Southern Oscillation and El Niño. Advances in Geophysics. 1985, 28A: 197–215. Bazilevskaya G., Usoskin I., Flückiger E., Harrison R., Desorgher L., Bütikofer R., Krainev M., Makhmutov V., Stozhkov Y., Svirzhevskaya A., Svirzhevsky N., Kovaltsov G. Cosmic ray induced ion production in the atmosphere. Space Sci. Rev. 2008, 137: 149–173. doi:10.1007/s11214- 008-9339-y. Mironova I., Aplin K., Arnold F., Bazilevskaya G., Harrison R., Krivolutsy A., Nicoll K., Rozanov E., Turunen E., Usoskin I. Energetic particle influence on the Earth’s atmosphere. Space Sci. Rev. 2015, 194: 1–96. doi:10.1007/s11214-015-0185-4. Miroshnichenko L.I. Solar cosmic rays: 75 years of research. Physics-Uspekhi. 2018, 61(4): 323–352. doi: https://doi.org/10.3367/UFNe.2017.03.038091. Mironova I., Bazilevskaya G., Kovaltsov G., Artamonov A., Rozanov E., Mishev A., Makhmutov V., Karagodin A., Golubenko K. Spectra of high energy electron precipitation and atmospheric ionization rates retrieval from balloon measurements. Science of the Total Environment. 2019, 693: 133242. https:doi.org/10.1016/j.scitotenv.2019.07.048. Usoskin, I.G., Kovaltsov G.A., Mironova I.A. Cosmic ray induced ionization model CRAC:CRII: An extension to the upper atmosphere. J. Geophys. Res. 2010, 115: D10302. doi:10.1029/2009JD013142. Usoskin, I.G., Kovaltsov G.A., Mironova I.A., Tylka A.J., Dietrich W.F. Ionization effect of solar particle GLE events in low and middle atmosphere. Atmospheric Chemistry and Physics. 2011, 11 (5): 1979–1988. doi:10.5194/acp-11-1979-2011. Tinsley B.A., Brown G.M., Scherrer P.H. Solar variability influences on weather and climate: possible connection through cosmic ray fluxes and storm intensification. J. Geophys. Res. 1989, 94: 14783–14792. Pudovkin M.I., Veretenenko S.V. Cloudiness decreases associated with Forbush-decreases of the galactic cosmic rays. J. Atmos. Terr. Phys. 1995, 57: 1349–1355. Svensmark H., Friis-Christensen E. 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Kristjansson J.E., Staple A., Kristiansen J., Kaas E. A new look at possible connection between solar activity, clouds and climate. Geophys. Res. Let. 2002, 29: 2107 doi:10.1029/2002GL015646. Harrison R.G., Carslaw K.S. Ion-aerosol-cloud processes in the lower atmosphere. Rev. Geophys. 2003, 41: 1012–1026. doi:10.1029/2002RG000114. Rycroft M.J., Nicoll K.A., Aplin K.L., Harrison R.G. Recent advances in global electric circuit coupling between the space environment and the troposphere. J. Atmos. Sol.-Terr. Phys. 2012, 90–91 (1):198–211, doi:10.1016/j.jastp.2012.03.015. Tinsley B.A., Rohrbaugh R.P., Hei M., Beard K.V. Effects of image charges on the scavenging of aerosol particles by cloud droplets and on droplet charging and possible ice nucleation processes. J. Atmos. Sci. 2000, 57: 2118–2134. Harrison R.G. Cloud formation and the possible significance of charge for atmospheric condensation and ice nuclei. Space Sci. Rev. 2000, 94: 381–396. Marsh N., Svensmark H. 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Arctic and Antarctic Research; Том 67, № 2 (2021); 177-207 Проблемы Арктики и Антарктики; Том 67, № 2 (2021); 177-207 2618-6713 0555-2648 10.30758/0555-2648-2021-67-2 южная осцилляция (ENSO) Earth’s atmosphere geoeffective solar wind high-energy solar protons (SPE) model computations ozone depletion planetary cloudiness quasi-biennial oscillation (QBO) solar UV irradiance Southern Oscillation (ENSO) Space weather атмосферная циркуляция высокоэнергичные солнечные протоны геоэффективный солнечный ветер квазидвухлетняя осцилляция (QBO) космическая погода модельные расчеты озоновая «дыра» планетарная облачность солнечное УФ-излучение info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2021 ftjaaresearch https://doi.org/10.30758/0555-2648-2021-67-2-177-20710.30758/0555-2648-2021-67-210.1007/s1121410.1007/s11214-015-0185-410.3367/UFNe.2017.03.03809110.1016/j.scitotenv.2019.07.04810.1029/2009JD01314210.5194/acp-11-1979-201110.1029/2001JD10.1029/1999GL900121 2024-05-31T03:22:51Z The review generalizes experimental data on the relationships between the solar activity agents (space weather) and atmosphere constituents. It is shown that high-energy solar protons (SPE) make a powerful impact on photo-chemical processes in the polar areas and, correspondingly, on atmospheric circulation and planetary cloudiness. Variations of the solar UV irradiance modulate the descent rate of the zonal wind in the equatorial stratosphere in the course of quasi-biennial oscillation (QBO), and thus control the total duration (period) of the QBO cycle and, correspondingly, the seasonal ozone depletion in the Antarctic. The geo-effective solar wind impacts on the atmospheric wind system in the entire Southern Polar region, and influences the dynamics of the Southern Oscillation (ENSO). В обзоре обобщены экспериментальные данные о влиянии космической погоды на земную атмосферу. Показано, что высокоэнергичные солнечные протоны (SPE) оказывают мощное воздействие на фотохимические процессы в полярных областях и, соответственно, на атмосферную циркуляцию и планетарную облачность. Вариации солнечного УФ-излучения моделируют скорость спуска зональных ветров в экваториальной стратосфере в ходе квазидвухлетней осцилляции (QBO) и контролируют, таким образом, общую продолжительность (период) QBO цикла и, соответственно, вариации общего содержания озона в Антарктике. Геоэффективный солнечный ветер воздействует на систему катабатических ветров во всей южной полярной области и влияет на динамику южной осцилляции (ENSO). Article in Journal/Newspaper Antarc* Antarctic Arctic Arctic and Antarctic Research Antarctic The Antarctic Arctic and Antarctic Research 67 2 177 207

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