arXivDaily arXiv每日学术速递 周一至周五更新
arXiv周末暂无论文更新,休息一下吧,周末愉快~~
arXiv 2602.19953astro-ph.SR
收藏

日冕空洞中冲击脊流相关的能量和质量传输

Energy and mass transport associated with impulsive spicular flows in solar coronal holes

Yunnan Observatories, Chinese Academy of Sciences(中国科学院云南天文台);University of Chinese Academy of Sciences(中国科学院大学);Indian Institute of Astrophysics(印度天体物理研究所);University of Sheffield(谢菲尔德大学);Eötvös Loránd University(罗兰大学)

Lei Ni, Jun Lin, Tanmoy Samanta, Guanchong Cheng, Yifu Wang, Robert Erdelyi

AI总结:

本研究通过磁流体动力学模拟和观测,揭示了日冕空洞中脊流上涌通过能量和质量传输加热日冕并维持太阳风的机制。

摘要:

太阳大气层从约5000-6000K的温度加热到约1-2MK的日冕的机制,已挑战天体物理学界约80年。同样的谜题也存在于恒星日冕加热中。在本研究中,我们通过磁流体动力学模拟与观测相结合,提出了关于太阳脊流及其对日冕影响的一系列发现,特别是在具有局部开放磁场线的日冕空洞环境中。我们发现,太阳表面的对流和湍流运动在低大气层中产生大量激波和小尺度磁重联。激波压缩和重联流出物的综合作用驱动了具有约300秒周期和约200-500公里宽度的脊流群。脊流上涌为低日冕提供平均质量通量超过10^-9 kg m^-2 s^-1,以维持日冕空洞中的太阳风。这些波持续触发新的局部慢模波和激波。这些波在低日冕提供10-100 W m^-2的能量通量,并通过热传导和压缩加热被耗散,以维持约1MK的日冕温度。研究结果还表明,观测到的向上的传播扰动(PDs)在极端紫外线(EUV)通带中是由脊流上涌和慢模波和激波共同引起的。我们的发现有助于理解日冕加热的长期问题以及日冕空洞区域太阳风的起源。

英文摘要:

How the solar atmosphere is heated from a temperature of about $5,000-6,000$\,K in the lower atmosphere to about $1-2$\,MK in the corona has challenged the astrophysical community for about 80 years. The same puzzle exists for the stellar coronae heating as well. In this study, we present a series of findings on solar spicules and their subsequent impact on the corona within a coronal hole environment, characterized by locally open magnetic field lines, combining insights from MHD simulations with observations. We find that the convective and turbulent motions around the solar surface cause plenty of shocks and small-scale magnetic reconnection in the lower atmosphere. The combined effects of shock compression and reconnection outflows then drive the formation of groups of spicules with a quasi-period of about $300$\,s and width of $\sim 200-500$\,km. The spicule upflows provide an averaged mass flux above $10^{-9}$\,kg\,m$^{-2}$\,s$^{-1}$ in the lower corona to sustain the solar wind in coronal holes, and they continuously trigger further new local slow-mode waves and shocks. These waves supply an energy flux of $10-100$\,W\,m$^{-2}$ in the lower corona, and they are dissipated by heat conduction and compression heating to sustain the corona temperature of about $1$\,MK. The results also indicate that the upward propagating disturbances (PDs) observed in extreme ultraviolet (EUV) passbands are caused by both spicule upflows and slow-mode waves and shocks. Our findings help to understand the long standing problem of coronal heating and the origin of solar winds in coronal hole regions.

机构、总结、中文摘要均由AI分析而来,可能存在错误,请以论文正文为准。

↑