太阳活动区漫射日冕等离子体的稳态加热

Gregory D. Fleishman, Alexey A. Kuznetsov and Gelu M. Nita
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引用次数: 0

摘要

日冕比太阳大气的下层——光球层和色球层要热得多。在太阳静止区,日冕温度高达1 MK,而在太阳活跃区,日冕温度高达数兆开尔文,这表明磁场在日冕加热中起着关键作用。这意味着理解日冕加热需要对活动区域的三维磁性结构进行可靠的建模,并得到观测结果的验证。在这里,我们利用三维建模、光学厚的陀螺谐振微波发射和光学薄的EUV发射之间的协同作用来(i)获得并验证活跃区域的最佳磁热模型;(ii)解开EUV发射的各种成分,即漫射成分、明亮环路、开场区域和在过渡区域产生的“苔藓”成分。令人惊讶的是,最好的热模型对应于高频能量释放事件,类似于稳态加热。我们的分析没有揭示元素丰度与标准日冕值的显著偏差。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Steady-state Heating of Diffuse Coronal Plasma in a Solar Active Region
The solar corona is much hotter than lower layers of the solar atmosphere—the photosphere and chromosphere. The coronal temperature is up to 1 MK in quiet Sun areas, while up to several megakelvins in active regions, which implies a key role of the magnetic field in coronal heating. This means that understanding coronal heating requires reliable modeling of the underlying 3D magnetic structure of an active region validated by observations. Here, we employ synergy between 3D modeling, optically thick gyroresonant microwave emission, and optically thin EUV emission to (i) obtain and validate the best magnetothermal model of the active region and (ii) disentangle various components of the EUV emission known as diffuse component, bright loops, open-field regions, and “moss” component produced at the transition region. Surprisingly, the best thermal model corresponds to high-frequency energy release episodes, similar to a steady-state heating. Our analysis did not reveal significant deviations of the elemental abundances from the standard coronal values.
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