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dc.contributor.authorPagano, Paolo
dc.contributor.authorMackay, Duncan Hendry
dc.contributor.authorPoedts, Stefaan
dc.date.accessioned2013-07-22T15:31:03Z
dc.date.available2013-07-22T15:31:03Z
dc.date.issued2013-06
dc.identifier.citationPagano , P , Mackay , D H & Poedts , S 2013 , ' Magnetohydrodynamic simulations of the ejection of a magnetic flux rope ' , Astronomy & Astrophysics , vol. 554 , A77 . https://doi.org/10.1051/0004-6361/201220947en
dc.identifier.issn0004-6361
dc.identifier.otherPURE: 60151155
dc.identifier.otherPURE UUID: ae1bba04-fea5-4c2d-9f88-9967e56d5f5a
dc.identifier.otherScopus: 84878982714
dc.identifier.otherORCID: /0000-0001-6065-8531/work/58055436
dc.identifier.urihttps://hdl.handle.net/10023/3855
dc.description.abstractContext. Coronal mass ejections (CME’s) are one of the most violent phenomena found on the Sun. One model to explain their occurrence is the flux rope ejection model. In this model, magnetic flux ropes form slowly over time periods of days to weeks. They then lose equilibrium and are ejected from the solar corona over a few hours. The contrasting time scales of formation and ejection pose a serious problem for numerical simulations. Aims. We simulate the whole life span of a flux rope from slow formation to rapid ejection and investigate whether magnetic flux ropes formed from a continuous magnetic field distribution, during a quasi-static evolution, can erupt to produce a CME. Methods. To model the full life span of magnetic flux ropes we couple two models. The global non-linear force-free field (GNLFFF) evolution model is used to follow the quasi-static formation of a flux rope. The MHD code ARMVAC is used to simulate the production of a CME through the loss of equilibrium and ejection of this flux rope. Results. We show that the two distinct models may be successfully coupled and that the flux rope is ejected out of our simulation box, where the outer boundary is placed at 2.5 R⊙. The plasma expelled during the flux rope ejection travels outward at a speed of 100 km s-1, which is consistent with the observed speed of CMEs in the low corona. Conclusions. Our work shows that flux ropes formed in the GNLFFF can lead to the ejection of a mass loaded magnetic flux rope in full MHD simulations. Coupling the two distinct models opens up a new avenue of research to investigate phenomena where different phases of their evolution occur on drastically different time scales.
dc.format.extent11
dc.language.isoeng
dc.relation.ispartofAstronomy & Astrophysicsen
dc.rights© ESO, 2013. This article was made open access through BIS funding.en
dc.subjectSunen
dc.subjectCoronal mass ejectionsen
dc.subjectCoronaen
dc.subjectMagnetic fieldsen
dc.subjectMagnetohydrodynamics (MHD)en
dc.subjectQ Scienceen
dc.subject.lccQen
dc.titleMagnetohydrodynamic simulations of the ejection of a magnetic flux ropeen
dc.typeJournal articleen
dc.contributor.sponsorScience & Technology Facilities Councilen
dc.description.versionPublisher PDFen
dc.contributor.institutionUniversity of St Andrews. Applied Mathematicsen
dc.contributor.institutionUniversity of St Andrews. School of Mathematics and Statisticsen
dc.identifier.doihttps://doi.org/10.1051/0004-6361/201220947
dc.description.statusPeer revieweden
dc.identifier.grantnumberST/K000950/1en


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