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Large-Scale Dynamics of the Convection Zone and Tachocline

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dc.creator Miesch Mark S.
dc.date 2005
dc.date.accessioned 2013-06-01T11:59:30Z
dc.date.available 2013-06-01T11:59:30Z
dc.date.issued 2013-06-01
dc.identifier http://www.livingreviews.org/lrsp-2005-1
dc.identifier http://www.doaj.org/doaj?func=openurl&genre=article&issn=16144961&date=2005&volume=2&issue=&spage=1
dc.identifier.uri http://koha.mediu.edu.my:8181/jspui/handle/123456789/8732
dc.description The past few decades have seen dramatic progress in our understanding of solar interior dynamics, prompted by the relatively new science of helioseismology and increasingly sophisticated numerical models. As the ultimate driver of solar variability and space weather, global-scale convective motions are of particular interest from a practical as well as a theoretical perspective. Turbulent convection under the influence of rotation and stratification redistributes momentum and energy,generating differential rotation, meridional circulation, and magnetic fields through hydromagnetic dynamo processes. In the solar tachocline near the base of the convection zone, strong angular velocity shear further amplifies fields which subsequently rise to the surface to form active regions. Penetrative convection, instabilities, stratified turbulence, and waves all add to the dynamical richness of the tachocline region and pose particular modeling challenges. In this article we review observational, theoretical, and computationalinvestigations of global-scale dynamics in the solar interior. Particular emphasis is placed on high-resolution global simulations of solar convection, highlighting what we have learned from them and how they may be improved.
dc.publisher Max Planck Institute for Solar System Research
dc.source Living Reviews in Solar Physics
dc.subject Convection
dc.subject Tachocline
dc.subject Differential rotation
dc.subject Meridional circulation
dc.subject Turbulence
dc.subject shear
dc.subject Dynamo theory
dc.title Large-Scale Dynamics of the Convection Zone and Tachocline


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