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首页> 外文期刊>The Astrophysical journal >EMERGENCE OF GRANULAR-SIZED MAGNETIC BUBBLES THROUGH THE SOLAR ATMOSPHERE. I. SPECTROPOLARIMETRIC OBSERVATIONS AND SIMULATIONS
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EMERGENCE OF GRANULAR-SIZED MAGNETIC BUBBLES THROUGH THE SOLAR ATMOSPHERE. I. SPECTROPOLARIMETRIC OBSERVATIONS AND SIMULATIONS

机译:穿过太阳大气的粒状磁泡的出现。一,分光观测与模拟

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摘要

We study a granular-sized magnetic flux emergence event that occurred in NOAA 11024 in 2009 July. The observations were made with the CRISP spectropolarimeter at the Swedish 1?m Solar Telescope achieving a spatial resolution of 014. Simultaneous full Stokes observations of the two photospheric Fe I lines at 630.2?nm and the chromospheric Ca II 854.2?nm line allow us to describe in detail the emergence process across the solar atmosphere. We report here on three-dimensional (3D) semi-spherical bubble events, where instead of simple magnetic footpoints, we observe complex semi-circular feet straddling a few granules. Several phenomena occur simultaneously, namely, abnormal granulation, separation of opposite-polarity legs, and brightenings at chromospheric heights. However, the most characteristic signature in these events is the observation of a dark bubble in filtergrams taken in the wings of the Ca II 854.2?nm line. There is a clear coincidence between the emergence of horizontal magnetic field patches and the formation of the dark bubble. We can infer how the bubble rises through the solar atmosphere as we see it progressing from the wings to the core of Ca II 854.2?nm. In the photosphere, the magnetic bubble shows mean upward Doppler velocities of 2?km?s–1 and expands at a horizontal speed of 4?km?s–1. In about 3.5?minutes it travels some 1100?km to reach the mid chromosphere, implying an average ascent speed of 5.2?km?s–1. The maximum separation attained by the magnetic legs is 66. From an inversion of the observed Stokes spectra with the SIR code, we find maximum photospheric field strengths of 480?G and inclinations of nearly 90° in the magnetic bubble interior, along with temperature deficits of up to 250?K at log τ = –2 and above. To aid the interpretation of the observations, we carry out 3D numerical simulations of the evolution of a horizontal, untwisted magnetic flux sheet injected in the convection zone, using the Bifrost code. The computational domain spans from the upper convection zone to the lower corona. In the modeled chromosphere, the rising flux sheet produces a large, cool, magnetized bubble. We compare this bubble with the observed ones and find excellent agreement, including similar field strengths and velocity signals in the photosphere and chromosphere, temperature deficits, ascent speeds, expansion velocities, and lifetimes.
机译:我们研究了2009年7月发生在NOAA 11024中的颗粒状磁通量出现事件。观测是使用CRISP分光偏振计在瑞典1?m太阳望远镜上完成的,其空间分辨率为014。同时对两个光球Fe I线在630.2?nm处和色球Ca II 854.2?nm线进行了全斯托克斯同步观察,这使我们能够详细描述整个太阳大气层的出现过程。我们在这里报告三维(3D)半球形气泡事件,在该事件中,我们观察到了跨越几个颗粒的复杂半圆形英尺,而不是简单的磁性英尺点。同时发生几种现象,即异常颗粒化,相反极性分支的分离以及色球层高度的增亮。但是,在这些事件中,最具特征性的特征是观察到在Ca II 854.2?nm谱线的机翼中滤出的暗气泡。在水平磁场斑块的出现与暗气泡的形成之间存在明显的巧合。我们可以推断出气泡是如何通过太阳大气层升起的,因为我们看到它从机翼一直延伸到Ca II 854.2nm的核心。在光球中,磁泡显示平均多普勒速度为2?km?s-1,并以4?km?s-1的水平速度扩展。在大约3.5分钟的时间内,它移动了大约1100公里,到达了色球中层,这意味着平均上升速度为5.2公里/秒-1。磁脚所能达到的最大间隔为66。从观察到的斯托克斯光谱与SIR代码的反演中,我们发现磁泡内部的最大光球场强度为480?G,倾角接近90°,并且存在温度缺陷。在logτ= –2及以上时,最大为250?K。为了帮助解释这些观察结果,我们使用Bifrost代码对注入对流区域的水平,未扭曲的水平磁通量板进行了3D数值模拟。计算域从上部对流区到下部电晕。在建模的色球层中,上升的通量表会产生一个大的,凉爽的磁化气泡。我们将该气泡与观察到的气泡进行了比较,并发现了极好的一致性,包括光球和色球中类似的场强和速度信号,温度不足,上升速度,膨胀速度和寿命。

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