论文标题
由颗粒状对流驱动的准周期性微喷雾剂,如高分辨率成像时观察到的10830Å
Quasi-periodic microjets driven by granular advection as observed with high-resolution imaging at He I 10830 Å
论文作者
论文摘要
使用高分辨率的窄带He I10830Å的GST滤波器图,我们对4个颗粒大小的微爆发进行了广泛的分析,这些微爆发是在He I10830Å带中显示为材料的温和弹出。分析通过来自AIA的EUV数据和HMI板上SDO的EUV数据和视线线图。微量爆发位于磁极性反转线(PIL)上,其根部被准确地追溯到晶间泳道。它们的持续时间不同,两个微暴发是重复的微喷枪,分别持续约50分钟和27分钟,而其他两个事件是单数,持续约5分钟。对于这两个微射线,它们在He I10830Å频段中是连续且经常性的,并且复发是准周期的,周期为5分钟。我们发现,仅在较长的持续时间微夹中观察到瞬时的共同空间EUV亮丽,并且对于两个奇异的微型爆发而没有EUV亮度。对于较长的持续时间微喷枪来说,必不可少的是,正磁场浓度的颗粒将磁场持续运输到PIL,取消相反的磁通量,并使两个微晶和下面的颗粒的底部以〜0.25和1.0 km/s的速度迁移。该观测结果支持准周期微型机流的磁重新连接方案,并进一步表明,重新连接连续生成多温成分,尤其是具有色层温度的凉爽成分。另外,正在进行的重新连接是由太阳内的P模式振荡调节的。
With high-resolution narrowband He I 10830 Å filtergrams from GST, we give an extensive analysis for 4 granular sized microeruptions which appear as the gentle ejection of material in He I 10830 Å band. The analysis was aided with the EUV data from AIA and line-of-sight magnetograms from HMI on board SDO. The microeruptions are situated on magnetic polarity inversion lines (PILs), and their roots are accurately traced down to intergranular lanes. Their durations are different, two microeruptions are repetitive microjets, lasting ~ 50 and 27 minutes respectively, while the other two events are singular, lasting ~ 5 minutes. For the two microjets, they are continuous and recurrent in He I 10830 Å band, and the recurrence is quasi-periodic with the period of ~ 5 minutes. We found that only transient co-spatial EUV brightenings are observed for the longer duration microjets and EUV brightenings are absent for the two singular microeruptions. What is essential to the longer duration microjets is that granules with the concentration of positive magnetic field persistently transport the magnetic field to the PILs, canceling the opposite magnetic flux and making the base of the two microjets and the underlying granules migrate with the speed of ~ 0.25 and 1.0 km/s. The observations support the scenario of magnetic reconnection for the quasi-periodic microjets and further show that the reconnection continuously generates multi-temperature components, especially the cool component with chromospheric temperature. In addition, the ongoing reconnection is modulated by p-mode oscillations inside the Sun.