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首页> 外文期刊>The Astrophysical journal >GLOBAL CORONAL SEISMOLOGY IN THE EXTENDED SOLAR CORONA THROUGH FAST MAGNETOSONIC WAVES OBSERVED BY STEREO SECCHI COR1
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GLOBAL CORONAL SEISMOLOGY IN THE EXTENDED SOLAR CORONA THROUGH FAST MAGNETOSONIC WAVES OBSERVED BY STEREO SECCHI COR1

机译:STEREO SECCHI COR1观测到的快速日冕波在日冕中的全球日冕地震学

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We present global coronal seismology for the first time, which allows us to determine inhomogeneous magnetic field strength in the extended corona. From the measurements of the propagation speed of a fast magnetosonic wave associated with a coronal mass ejection (CME) and the coronal background density distribution derived from the polarized radiances observed by the STEREO SECCHI COR1, we determined the magnetic field strengths along the trajectories of the wave at different heliocentric distances. We found that the results have an uncertainty less than 40%, and are consistent with values determined with a potential field model and reported in previous works. The characteristics of the coronal medium we found are that (1) the density, magnetic field strength, and plasma β are lower in the coronal hole region than in streamers; (2) the magnetic field strength decreases slowly with height but the electron density decreases rapidly so that the local fast magnetosonic speed increases while plasma β falls off with height; and (3) the variations of the local fast magnetosonic speed and plasma β are dominated by variations in the electron density rather than the magnetic field strength. These results imply that Moreton and EIT waves are downward-reflected fast magnetosonic waves from the upper solar corona, rather than freely propagating fast magnetosonic waves in a certain atmospheric layer. In addition, the azimuthal components of CMEs and the driven waves may play an important role in various manifestations of shocks, such as type II radio bursts and solar energetic particle events.
机译:我们首次介绍了全球日冕地震学,这使我们能够确定扩展电晕中的不均匀磁场强度。通过测量与冠状物质抛射(CME)相关的快速磁声波的传播速度以及从STEREO SECCHI COR1观测到的极化辐射得出的冠状背景密度分布,我们确定了沿轨道的磁场强度在不同的日心中心距离处发生波动。我们发现,结果的不确定度小于40%,并且与使用潜在田间模型确定并在先前工作中报告的值一致。我们发现冠状介质的特征是:(1)冠状孔区域的密度,磁场强度和血浆β均低于流光; (2)磁场强度随着高度的增加而缓慢减小,但电子密度迅速减小,从而局部快速的磁声速增加,而等离子体β随高度下降。 (3)局部快磁速和等离子体β的变化主要由电子密度的变化而不是磁场强度的变化决定。这些结果表明,Moreton和EIT波是来自上部太阳日冕的向下反射的快速磁声波,而不是在某个大气层中自由传播的快速磁声波。此外,CME和驱动波的方位分量可能在各种形式的冲击中起重要作用,例如II型无线电脉冲和太阳高能粒子事件。

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