MAGNETIC-FIELD EVOLUTION DURING PROMINENCE ERUPTIONS AND 2-RIBBON FLARES

被引:133
作者
PRIEST, ER [1 ]
FORBES, TG [1 ]
机构
[1] SPACE SCI CTR,SCI ENGN RES BLDG,DURHAM,NH 03824
关键词
D O I
10.1007/BF00153054
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
Simple models for the MHD eruption of a solar prominence are presented, in which the prominence is treated as a twisted magnetic flux tube that is being repelled from the solar surface by magnetic pressure forces. The effects of different physical assumptions to deal with this magneto-hydrodynamically complex phenomenon are evaluated, such as holding constant the prominence current, radius, flux or twist or modelling the prominence as a current sheet. Including a background magnetic field allows the prominence to be in equilibrium initially with an Inverse Polarity and then to erupt due to magnetic non-equilibrium when the background magnetic field is too small or the prominence twist is too great. The electric field at the neutral point below the prominence rapidly increases to a maximum value and then declines. Including the effect of gravity also allows an equilibrium with Normal Polarity to exist. Finally, an ideal MHD solution is found which incorporates self-consistently a current sheet below the prominence and which implies that a prominence will still erupt and form a current sheet even if no reconnection occurs. When reconnection is allowed it is, therefore, driven by the eruption. © 1990 Kluwer Academic Publishers.
引用
收藏
页码:319 / 350
页数:32
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