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首页> 外文期刊>The Astrophysical Journal. Letters >IMAGING AND SPECTROSCOPIC OBSERVATIONS OF MAGNETIC RECONNECTION AND CHROMOSPHERIC EVAPORATION IN A SOLAR FLARE
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IMAGING AND SPECTROSCOPIC OBSERVATIONS OF MAGNETIC RECONNECTION AND CHROMOSPHERIC EVAPORATION IN A SOLAR FLARE

机译:太阳耀斑中磁重合和色球蒸发的成像和光谱观察

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摘要

Magnetic reconnection is believed to be the dominant energy release mechanism in solar flares. The standard flare model predicts both downward and upward outflow plasmas with speeds close to the coronal Alfven speed. Yet, spectroscopic observations of such outflows, especially the downflows, are extremely rare. With observations of the newly launched Interface Region Imaging Spectrograph (IRIS), we report the detection of a greatly redshifted (similar to 125 km s(-1) along the line of sight) Fe XXI 1354.08.angstrom emission line with a similar to 100 km s(-1) nonthermal width at the reconnection site of a flare. The redshifted Fe XXI feature coincides spatially with the loop-top X-ray source observed by RHESSI. We interpret this large redshift as the signature of downward-moving reconnection outflow/hot retracting loops. Imaging observations from both IRIS and the Atmospheric Imaging Assembly (AIA) on board the Solar Dynamics Observatory also reveal the eruption and reconnection processes. Fast downward-propagating blobs along these loops are also found from cool emission lines (e. g., Si IV, O IV, C II, Mg II) and images of AIA and IRIS. Furthermore, the entire Fe XXI line is blueshifted by similar to 260 km s(-1) at the loop footpoints, where the cool lines mentioned above all exhibit obvious redshift, a result that is consistent with the scenario of chromospheric evaporation induced by downward-propagating nonthermal electrons from the reconnection site.
机译:磁重联被认为是太阳耀斑中主要的能量释放机制。标准耀斑模型可预测向下和向上流出的等离子体,其速度接近日冕Alfven速度。然而,这种流出物,特别是流出物的光谱观察极为罕见。借助新近推出的界面区域成像光谱仪(IRIS)的观测,我们报告发现检测到一条极大的红移(类似于沿视线的125 km s(-1))Fe XXI 1354.08。埃发射线,与100火炬再连接点的km s(-1)非热宽度。红移的Fe XXI特征在空间上与RHESSI观测到的环顶X射线源重合。我们将这个大的红移解释为向下移动的重新连接流出/热缩回环路的标志。太阳动力天文台上的IRIS和大气成像组件(AIA)的成像观测结果也揭示了火山喷发和重新连接的过程。还从冷的发射线(例如,Si IV,O IV,C II,Mg II)以及AIA和IRIS的图像中发现沿着这些环路的快速向下传播的斑点。此外,整个Fe XXI线在回路脚点都发生了260 km s(-1)的蓝移,其中上述冷线都表现出明显的红移,这一结果与下沉引起的色球蒸发的情况是一致的。从重新连接位置传播非热电子。

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