YNAO OpenIR  > 选址与日冕观测组
日冕喷流及波动的研究
其他题名Studies of the Coronal Jets and Waves
苗玉虎
学位类型博士
导师刘煜
2019-07-01
学位授予单位中国科学院大学
学位授予地点北京
学位专业天体物理
关键词喷流 日冕波 暗条 日冕物质抛射 耀斑
摘要本论文主要通过高分辨、多波段和多角度的数据对日冕喷流和日冕波动现象进行了研究。本论文共分六个部分。第一部分引言,主要介绍与太阳相关的一些基本爆发活动,重点介绍喷流和日冕波相关背景;第二章主要介绍本工作所使用的数据和设备;第三章至第五章,主要介绍在攻读博士期间所做的相关研究工作。第六章是总结与展望。 本论文在第三章和第五章中着重介绍喷流方面的研究。本论文在第三章中研究一个爆裂喷流及其引发的双日冕物质抛射(CME)现象,即一个喷流状日冕物质抛射和一个泡状日冕物质抛射。该事件是目前观测到的第二例由爆裂喷流爆发所引发的双日冕物质抛射事件。该爆裂喷流底部有一微暗条也随喷流一起爆发。泡状喷流的形成一般认为有两种可能原因,一种是由于微暗条爆发内部磁重联导致的,另一种可能性是由于日冕高层的磁场重构导致的;值得一提的是,该爆裂喷流爆发上升阶段,前端产生了一个极紫外(extreme-ultraviolet(EUV))波。本论文也简略探讨了喷流与日冕波的关系。通过多角度、高分辨和多波段数据对该事件进行了全面分析,该事件对研究日冕磁场结构重组具有重要意义。 在本论文第四章中对日冕波进行了研究。通常认为日冕极紫外波(EUV wave)和准周期快模磁声波(quasi-periodic fast-propagating (QFP) magnetosonic wave)的触发机制是不同的。一般认为EUV波与日冕物质抛射关系密切,QFP波与耀斑爆发有重要联系。但在本章中,在同一个事件爆发中,发现了EUV波和QFP波同时爆发的现象,并且EUV波的波前与QFP波列的第一个波前在空间观测上是同一个波前。此次事件为我们提供了一个非常好的机会去探测这两种波的爆发机制和起源。在日面上观测到的宽带脉冲可以认为是活塞式激波,这种波一般是由日冕物质抛射引起的,宽带脉冲沿着扇形冕环传播,由于色散,在扇形冕环上形成了QFP波列,由于STEREO卫星观测到了对应的日冕物质抛射现象,因此,我们认为该QFP波与日冕物质抛射有关。 在本论文的第五章中研究了活动区AR11166边缘处一个重复喷流事件。该事件最初由一个新浮现的带有负极性磁场的卫星黑子触发。负极性卫星黑子与先前存在的正极性主黑子的磁场发生对消导致重复喷流事件。在此过程中,卫星黑子不断移动,在移动过程中与周边新磁浮现的同极性磁通量发生汇聚融合。此次重复喷流事件共统计了 37次独立喷流,并将这37个喷流事件分成两类:爆裂喷流和标准喷流,并给出了判断依据。通过研究爆裂喷流和标准喷流在光球上磁场运动和演化,表明爆裂喷流爆发时,磁场的扭缠运动和剪切运动更剧烈一些。研究还表明,爆裂喷流爆发时,能够释放更多的能量,并且爆发的速度和规模比标准喷流的速度要快,规模更大。爆裂喷流爆发时往往伴随耀斑或者底部增亮,而标准喷流就没有如此明显的特征。 总的来说,本论文主要对喷流和日冕波的爆发机制做了研究和探讨。本论文研究成果如下:1、喷流与小张角EUV波密切联系;2、爆裂喷流导致双CME事件又有新的证据,证明并完善了申远灯、刘煜、苏江涛和邓元勇等人的模型[1]; 3、爆裂喷流和标准喷流之间存在较大区别; 4、EUV波与QFP波触发机制的新发现。以上研究结果对完善喷流模型、日冕物质抛射的类型和日冕波的起源和演化具有重要意义。
其他摘要By using the high resolution, multi-wavelength and multi-angle observation data, we study coronal jets and coronal waves in this thesis. The thesis is divided into six chapters. The first chapter is the introduction of solar physics. Especially, it mainly focuses on the background of the coronal jets and the coronal waves. The second chapter mainly introduces the data and instruments. From the third to the fifth chapters, these chapters mainly explain the work I did during my PhD. The last chapter makes the summary and prospect. In the third and the fifth chapters, we mainly focus on the research of the coronal jets. In the third chapter, we study a blowout jet eruption event. Interestingly, the blowout jet eruption simultaneously triggers two coronal mass ejections (CMEs), namely, one is a jet-like CME and the other one is a bubble-like CME. This event is the second double-CME event up to now. The bubble-like CME might either be produced by the internal reconnection during the mini-filament ejection or the reconstruction of the high coronal fields. It is worth mentioning that a EUV wave is generated at the front of the blowout jet during the rising phase of the blowout jet. The relationship between the blowout jet and the coronal wave is also discussed briefly in the thesis. By using multi-angle, high resolution and multi-wavelength data to analyze, this kind of event is very important for investigating the reconstruction of the coronal magnetic fields. The coronal waves are presented in the fourth chapter of the thesis. The triggering mechanisms of the EUV waves and the QFP waves were generally thought to be different. In general, the large-scale EUV waves are driven by CMEs, while the QFP waves are believed to be associated with the accompanied flares. In the fourth chapter, we study a EUV wave and a QFP wave excited simultaneously in a CME/flare eruption event. The wavefront of the EUV wave is cospatial with the first wavefront of the QFP wave train. The co-existence of the two wave phenomena offers an excellent opportunity to explore their driving mechanisms in one solar eruption event. The broadband pulse could be regarded as a piston-driven shock wave as observed in the present case, which further dispersively evolved into the QFP wave along with the fan-structure coronal loops. In general, the shock waves are caused by CMEs. Due to the two STEREO satellites captured the counterpart CME, hence, we confirm that the QFP wave has a tight relationship with the CME. In the fifth chapter of the thesis, a recurrent jet event is studied. The event is initially from a new small satellite with negative flux and triggers the recurrent jet event. The cancellation is undergoing between the negative patch and the pre-existing positive polarity. During the stage, the small satellite sunspot exhibits motion toward the southeast of AR11166 and merges with the emerging flux. The recurrent jet event includes thirty-seven jets. All of the jets can be classified into two types, the blowout jet and the standard jet. We also try to define the criteria for judging the standard and blowout coronal jets. By studying the magnetic field motion and evolution of the blowout jet and the standard jet on the photosphere, it suggests that the twistingand shearing motions of the magnetic field are more intense when the blowout jet erupts. Thestudy also shows that blowout jets release more energy when they erupt. They are faster andhave a larger scale than standard jets. Blowout jets often accompany with flares or bottombrightening, while standard jets do not have such obvious characteristics. Above all, the thesis mainly focuses on the studies and discussions of the coronal jets andthe coronal waves. The research results of the thesis are as follows: 1. The jet has a closerelationship with the small angle EUV wave; 2. a blowout jet leads to a double-CME event,which is found new evidence and improves the jet model of the Shen, Liu, Su and Deng; 3. thereare many differences between a blowout jet and a standard jet; 4. The new trigger mechanismof the EUV waves and the QFP waves is found. These studies are very important for improving the model of the jet. They are also very important for studying the origin and evolution of the coronal waves.
学科领域天文学 ; 太阳与太阳系 ; 太阳物理学
学科门类理学 ; 理学::天文学
页数124
语种中文
文献类型学位论文
条目标识符http://ir.ynao.ac.cn/handle/114a53/25447
专题选址与日冕观测组
作者单位中国科学院云南天文台
第一作者单位中国科学院云南天文台
推荐引用方式
GB/T 7714
苗玉虎. 日冕喷流及波动的研究[D]. 北京. 中国科学院大学,2019.
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