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观测太阳爆发喷流中的开尔文-亥姆霍兹不稳定性。

Observing Kelvin-Helmholtz instability in solar blowout jet.

作者信息

Li Xiaohong, Zhang Jun, Yang Shuhong, Hou Yijun, Erdélyi Robert

机构信息

CAS Key Laboratory of Solar Activity, National Astronomical Observatories, Chinese Academy of Sciences, Beijing, 100101, China.

School of Astronomy and Space Science, University of Chinese Academy of Sciences, Beijing, 100049, China.

出版信息

Sci Rep. 2018 May 25;8(1):8136. doi: 10.1038/s41598-018-26581-4.

Abstract

Kelvin-Helmholtz instability (KHI) is a basic physical process in fluids and magnetized plasmas, with applications successfully modelling e.g. exponentially growing instabilities observed at magnetospheric and heliospheric boundaries, in the solar or Earth's atmosphere and within astrophysical jets. Here, we report the discovery of the KHI in solar blowout jets and analyse the detailed evolution by employing high-resolution data from the Interface Region Imaging Spectrograph (IRIS) satellite launched in 2013. The particular jet we focus on is rooted in the surrounding penumbra of the main negative polarity sunspot of Active Region 12365, where the main body of the jet is a super-penumbral structure. At its maximum, the jet has a length of 90 Mm, a width of 19.7 Mm, and its density is about 40 times higher than its surroundings. During the evolution of the jet, a cavity appears near the base of the jet, and bi-directional flows originated from the top and bottom of the cavity start to develop, indicating that magnetic reconnection takes place around the cavity. Two upward flows pass along the left boundary of the jet successively. Next, KHI develops due to a strong velocity shear (∼204 km s) between these two flows, and subsequently the smooth left boundary exhibits a sawtooth pattern, evidencing the onset of the instability.

摘要

开尔文 - 亥姆霍兹不稳定性(KHI)是流体和磁化等离子体中的一种基本物理过程,其应用成功地模拟了例如在磁层和日球层边界、太阳或地球大气层以及天体物理喷流中观测到的指数增长的不稳定性。在此,我们报告在太阳爆发喷流中发现了KHI,并利用2013年发射的界面区域成像光谱仪(IRIS)卫星的高分辨率数据分析了其详细演化过程。我们关注的特定喷流起源于活动区12365主要负极性黑子周围的半影区,喷流主体是一个超半影结构。喷流在最大时,长度为90Mm,宽度为19.7Mm,其密度约为周围环境的40倍。在喷流演化过程中,喷流底部附近出现一个空洞,源自空洞顶部和底部的双向流动开始发展,这表明在空洞周围发生了磁重联。两股向上的流动相继沿着喷流的左边界通过。接下来,由于这两股流动之间存在强烈的速度剪切(约204km/s),KHI开始发展,随后光滑的左边界呈现出锯齿状图案,证明了不稳定性的开始。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0437/5970241/0bf2db0562a3/41598_2018_26581_Fig1_HTML.jpg

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