Solar turbulent dynamo near convective overshoot layer and radiative tachocline

In order to extend the abilities of the αΩ-dynamo model to explain the observed regularities and anomalies of the solar magnetic activity, the magnetic quenching of the α-effect were included in the model, and newest helioseismically determined inner rotation of the Sun has been used. Allowance for...

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Бібліографічні деталі
Опубліковано в: :Кинематика и физика небесных тел
Дата:2005
Автор: Kryvodubskyj, V.N.
Формат: Стаття
Мова:English
Опубліковано: Головна астрономічна обсерваторія НАН України 2005
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Онлайн доступ:https://nasplib.isofts.kiev.ua/handle/123456789/79616
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Назва журналу:Digital Library of Periodicals of National Academy of Sciences of Ukraine
Цитувати:Solar turbulent dynamo near convective overshoot layer and radiative tachocline / V.N. Kryvodubskyj // Кинематика и физика небесных тел. — 2005. — Т. 21, № 5-додаток. — С. 117-123. — Бібліогр.: 51 назв. — англ.

Репозитарії

Digital Library of Periodicals of National Academy of Sciences of Ukraine
id nasplib_isofts_kiev_ua-123456789-79616
record_format dspace
spelling Kryvodubskyj, V.N.
2015-04-03T15:30:07Z
2015-04-03T15:30:07Z
2005
Solar turbulent dynamo near convective overshoot layer and radiative tachocline / V.N. Kryvodubskyj // Кинематика и физика небесных тел. — 2005. — Т. 21, № 5-додаток. — С. 117-123. — Бібліогр.: 51 назв. — англ.
0233-7665
https://nasplib.isofts.kiev.ua/handle/123456789/79616
In order to extend the abilities of the αΩ-dynamo model to explain the observed regularities and anomalies of the solar magnetic activity, the magnetic quenching of the α-effect were included in the model, and newest helioseismically determined inner rotation of the Sun has been used. Allowance for the radial inhomogeneity of turbulent velocity in derivations of the helicity parameter resulted in a change of sign of the α-effect from positive to negative in the northern hemisphere near the bottom of the solar convection zone (SCZ). The change of sign is very important for direction of Parker’s dynamo-waves propagation and for parity of excited magnetic fields. The period of the dynamo-wave calculated with taking into account the magnetic α-quenching is about seven years, that agrees by order of magnitude with the observed mean duration of the sunspot cycles. Using the modern helioseismology data to define dynamo-parameters, we conclude that north–south asymmetry should exist in the meridional field. The calculated configuration of the net meridional field is likely to explain the magnetic anomaly of polar fields (the apparent magnetic “monopole”) observed near the maxima of solar cycles.
Author thanks L. L. Kitchatinov for a useful discussion.
en
Головна астрономічна обсерваторія НАН України
Кинематика и физика небесных тел
MS2: Physics of Solar Atmosphere
Solar turbulent dynamo near convective overshoot layer and radiative tachocline
Article
published earlier
institution Digital Library of Periodicals of National Academy of Sciences of Ukraine
collection DSpace DC
title Solar turbulent dynamo near convective overshoot layer and radiative tachocline
spellingShingle Solar turbulent dynamo near convective overshoot layer and radiative tachocline
Kryvodubskyj, V.N.
MS2: Physics of Solar Atmosphere
title_short Solar turbulent dynamo near convective overshoot layer and radiative tachocline
title_full Solar turbulent dynamo near convective overshoot layer and radiative tachocline
title_fullStr Solar turbulent dynamo near convective overshoot layer and radiative tachocline
title_full_unstemmed Solar turbulent dynamo near convective overshoot layer and radiative tachocline
title_sort solar turbulent dynamo near convective overshoot layer and radiative tachocline
author Kryvodubskyj, V.N.
author_facet Kryvodubskyj, V.N.
topic MS2: Physics of Solar Atmosphere
topic_facet MS2: Physics of Solar Atmosphere
publishDate 2005
language English
container_title Кинематика и физика небесных тел
publisher Головна астрономічна обсерваторія НАН України
format Article
description In order to extend the abilities of the αΩ-dynamo model to explain the observed regularities and anomalies of the solar magnetic activity, the magnetic quenching of the α-effect were included in the model, and newest helioseismically determined inner rotation of the Sun has been used. Allowance for the radial inhomogeneity of turbulent velocity in derivations of the helicity parameter resulted in a change of sign of the α-effect from positive to negative in the northern hemisphere near the bottom of the solar convection zone (SCZ). The change of sign is very important for direction of Parker’s dynamo-waves propagation and for parity of excited magnetic fields. The period of the dynamo-wave calculated with taking into account the magnetic α-quenching is about seven years, that agrees by order of magnitude with the observed mean duration of the sunspot cycles. Using the modern helioseismology data to define dynamo-parameters, we conclude that north–south asymmetry should exist in the meridional field. The calculated configuration of the net meridional field is likely to explain the magnetic anomaly of polar fields (the apparent magnetic “monopole”) observed near the maxima of solar cycles.
issn 0233-7665
url https://nasplib.isofts.kiev.ua/handle/123456789/79616
citation_txt Solar turbulent dynamo near convective overshoot layer and radiative tachocline / V.N. Kryvodubskyj // Кинематика и физика небесных тел. — 2005. — Т. 21, № 5-додаток. — С. 117-123. — Бібліогр.: 51 назв. — англ.
work_keys_str_mv AT kryvodubskyjvn solarturbulentdynamonearconvectiveovershootlayerandradiativetachocline
first_indexed 2025-12-07T15:22:43Z
last_indexed 2025-12-07T15:22:43Z
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