...
首页> 外文期刊>The Astrophysical journal >ANALYSIS OF CORONAL RAIN OBSERVED BY IRIS, HINODE/SOT, AND SDO/AIA: TRANSVERSE OSCILLATIONS, KINEMATICS, AND THERMAL EVOLUTION
【24h】

ANALYSIS OF CORONAL RAIN OBSERVED BY IRIS, HINODE/SOT, AND SDO/AIA: TRANSVERSE OSCILLATIONS, KINEMATICS, AND THERMAL EVOLUTION

机译:IRIS,HINODE / SOT和SDO / AIA观测到的日冕雨的分析:横向振荡,运动学和热演化

获取原文
   

获取外文期刊封面封底 >>

       

摘要

Coronal rain composed of cool plasma condensations falling from coronal heights along magnetic field lines is a phenomenon occurring mainly in active region coronal loops. Recent high-resolution observations have shown that coronal rain is much more common than previously thought, suggesting its important role in the chromosphere-corona mass cycle. We present the analysis of MHD oscillations and kinematics of the coronal rain observed in chromospheric and transition region lines by the Interface Region Imaging Spectrograph (IRIS), the Hinode Solar Optical Telescope (SOT), and the Solar Dynamics Observatory (SDO) Atmospheric Imaging Assembly (AIA). Two different regimes of transverse oscillations traced by the rain are detected: small-scale persistent oscillations driven by a continuously operating process and localized large-scale oscillations excited by a transient mechanism. The plasma condensations are found to move with speeds ranging from few km s?1 up to 180 km s?1 and with accelerations largely below the free-fall rate, likely explained by pressure effects and the ponderomotive force resulting from the loop oscillations. The observed evolution of the emission in individual SDO/AIA bandpasses is found to exhibit clear signatures of a gradual cooling of the plasma at the loop top. We determine the temperature evolution of the coronal loop plasma using regularized inversion to recover the differential emission measure (DEM) and by forward modeling the emission intensities in the SDO/AIA bandpasses using a two-component synthetic DEM model. The inferred evolution of the temperature and density of the plasma near the apex is consistent with the limit cycle model and suggests the loop is going through a sequence of periodically repeating heating-condensation cycles.
机译:由沿磁场线从日冕高度下降的冷等离子体凝结物构成的日冕雨主要在活动区域​​日冕环中发生。最近的高分辨率观测表明日冕雨比以前认为的要普遍得多,表明日冕雨在色球层-电晕质量循环中的重要作用。我们介绍了通过界面区域成像光谱仪(IRIS),日出阳极太阳光学望远镜(SOT)和太阳动力学天文台(SDO)大气成像组件在色球层和过渡区域线中观测到的MHD振荡和运动的运动学(AIA)。检测到由雨水追踪的两种不同的横向振荡状态:由连续运行过程驱动的小规模持续振荡,以及由瞬变机制激发的局部大范围振荡。发现等离子凝结的移动速度从几公里s?1到180 km s?1不等,并且加速度大大低于自由落体速率,这很可能是由于压力效应和回路振荡产生的质动力所解释的。发现在单个SDO / AIA带通中观察到的发射演化显示出在回路顶部等离子体逐渐冷却的清晰特征。我们使用正则化反演来恢复差分发射量度(DEM),并使用两组分合成DEM模型对SDO / AIA带通中的发射强度进行正向建模,从而确定日冕环等离子体的温度演变。推断出顶点附近等离子体的温度和密度的变化与极限循环模型一致,这表明循环正在经历一系列周期性重复的加热-冷凝循环。

著录项

获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号