Characterizing Chromospheric Condensation with High-cadence Si iv Observations from IRIS

Chunming Zhu, Willow Reed, Alysa Derks and Dana Longcope
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Abstract

Chromospheric flare ribbons are believed to result from coronal magnetic energy released by reconnection and propagating down to the cooler, lower atmosphere. They offer an opportunity to study flare reconnection using chromospheric observations at a spatial and temporal resolution higher than typically available by direct coronal observation. Transient downflows, known as chromospheric condensations (CCs), often occur at the leading edge of a ribbon as a prompt response to the energy input. These have properties that have recently been shown to relate to the coronal energy release process driving them. We use a set of IRIS observations of flare ribbons, made at high cadence in the sit-and-stare mode, to identify and analyze a sample of 134 CC episodes. Among this sample, 132 episodes have at least one time frame that exhibited a double-Gaussian profile. Clear CC appears to occur in only about one fifth of all ribbon pixels, indicating that flare energy release is necessary but not sufficient for producing the characteristic form of CC. We find that condensation pixels form clusters averaging 1 arcsec in extent, all undergoing similar and concurrent time evolution. This suggests that coronal reconnection and associated energy release occur in localized patches whose spatial extent maps to around 1 arcsec in the chromosphere.
用IRIS高节奏Si - iv观测表征色球凝结
色球耀斑带被认为是由重联释放的日冕磁能向较冷的低层大气传播而产生的。它们提供了一个利用色球观测来研究耀斑重联的机会,其空间和时间分辨率比直接日冕观测通常更高。瞬态下流,称为色球凝聚(CCs),经常发生在条带的前缘,作为对能量输入的迅速响应。这些特性最近被证明与驱动它们的日冕能量释放过程有关。我们使用IRIS在高节奏的静坐-凝视模式下对耀斑带进行观测,以识别和分析134个CC事件的样本。在这个样本中,132集至少有一个时间框架表现出双高斯分布。清晰的CC似乎只发生在所有带状像素的五分之一左右,这表明耀斑能量释放是必要的,但不足以产生CC的特征形式。我们发现凝结像素形成的团簇平均范围为1弧秒,所有的团簇都经历了相似和并发的时间演化。这表明日冕重联和相关的能量释放发生在局部斑块中,其空间范围在色球层中约为1弧秒。
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