Multiwavelength study of on-disk coronal-hole jets with IRIS and SDO observations

Koletti Myrto, Gontikakis Costis, Patsourakos Spiros, Tsinganos Kanaris
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Abstract

Solar jets are an important field of study, as they may contribute to the mass and energy transfer from the lower to the upper atmosphere. We use the Interface Region Imaging Spectrograph (IRIS) and Solar Dynamic Observatory (SDO) observations to study two small-scale jets (jet 1 and jet 2) originating in the same on-disk coronal hole observed in October 2013. We combine dopplergrams, intensity maps, and line width maps derived from IRIS Si IV 1393.755Å spectra along with images from the Atmospheric Imaging Assembly (AIA) on SDO to describe the dynamics of the jets. Images from AIA, with the use of the emission measure loci technique and rectangular differential emission measure (DEM) distributions, provide estimations of the plasma temperatures. We used the O IV spectral lines from IRIS to derive electron densities. For jet 1, the SDO images show a small mini-filament 2 minutes before the jet eruption, while jet 2 originates at a pre-existing coronal bright point. The analysis of asymmetric spectral profiles of the Si IV and 1402.770 lines reveals the existence of two spectral components with inversely dependant 1393.755 ratios at both regions. One of the components can be related to the background plasma emission originating outside the jet, while the secondary component represents higher-energy plasma flows associated with the jets. Both jets exhibit high densities of the order of 1011 $ at their base and 1010 cm$^ $ at the spire, respectively, as well as similar average nonthermal velocities of sim 50-60 km/s. However, the two jets show differences in their length, duration, and plane-of-sky velocity. Finally, the DEM analysis reveals that both jets exhibit multithermal distributions. This work presents a comprehensive description of the thermal parameters and the dynamic evolution of two jets. The locations of the asymmetric profiles possibly indicate the areas of energy release triggering the jets.
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利用 IRIS 和 SDO 观测对盘面日冕洞喷流进行多波长研究
太阳喷流是一个重要的研究领域,因为它们可能有助于质量和能量从低层大气向高层大气的转移。我们利用界面区域成像光谱仪(IRIS)和太阳动力学天文台(SDO)的观测数据研究了源自2013年10月观测到的同一个日冕盘上的日冕洞的两个小尺度喷流(喷流1和喷流2)。我们将从 IRIS Si IV 1393.755Å 光谱中获得的多普勒图、强度图和线宽图与 SDO 上大气成像组件 (AIA) 的图像结合起来,以描述喷流的动态。大气成像组件(AIA)的图像利用发射测量定位技术和矩形差分发射测量(DEM)分布,提供了等离子体温度的估计值。我们利用 IRIS 的 O IV 光谱线推算电子密度。对于喷流 1,SDO 图像显示在喷流爆发前 2 分钟有一个小的迷你纤丝,而喷流 2 则起源于一个预先存在的日冕亮点。对 Si IV 和 1402.770 线不对称光谱剖面的分析表明,在两个区域都存在两个光谱成分,其 1393.755 比值成反比。其中一个成分与喷流外的背景等离子体发射有关,而另一个成分则代表了与喷流相关的高能等离子体流。两个喷流的密度都很高,在基部分别为 1011 美元,在尖顶分别为 1010 cm$^ 美元,平均非热速度也相似,都为模拟 50-60 公里/秒。然而,这两个喷流在长度、持续时间和天面速度上都存在差异。最后,DEM 分析表明,两个喷流都呈现多热分布。这项工作全面描述了两个喷流的热参数和动态演变过程。
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