Spectral Evolution of an Eruptive Polar Crown Prominence With IRIS Observations

Prominence eruption is closely related to coronal mass ejections and is an important topic in solar physics. Spectroscopic observation is an effective way to explore the plasma properties, but the spectral observations of eruptive prominences are rare. In this paper we will introduce an eruptive pol...

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Main Authors: Jianchao Xue , Hui Li , Yang Su 
Format: Article
Language:English
Published: Frontiers Media S.A. 2021-09-01
Series:Frontiers in Physics
Subjects:
Online Access:https://www.frontiersin.org/articles/10.3389/fphy.2021.750097/full
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author Jianchao Xue 
Hui Li 
Hui Li 
Yang Su 
Yang Su 
author_facet Jianchao Xue 
Hui Li 
Hui Li 
Yang Su 
Yang Su 
author_sort Jianchao Xue 
collection DOAJ
description Prominence eruption is closely related to coronal mass ejections and is an important topic in solar physics. Spectroscopic observation is an effective way to explore the plasma properties, but the spectral observations of eruptive prominences are rare. In this paper we will introduce an eruptive polar crown prominence with spectral observations from the Interface Region Imaging Spectrograph (IRIS), and try to explain some phenomena that are rarely reported in previous works. The eruptive prominence experiences a slow-rise and fast-rise phase, while the line-of-sight motions of the prominence plasma could be divided into three periods: 2 hours before the fast-rise phase, opposite Doppler shifts are found at the two sides of the prominence axis; then, red shifts dominate the prominence gradually; in the fast-rise phase, the prominence gets to be blue-shifted. During the second period, a faint component appears in Mg ii k window with a narrow line width and a large red shift. A faint region is also found in AIA 304Å images along the prominence spine, and the faint region gets darker during the expansion of the spine. We propose that the opposite Doppler shifts in the first period is a feature of the polar crown prominence that we studied. The red shifts in the second period are possibly due to mass drainage during the elevation of the prominence spine, which could accelerate the eruption in return. The blue shifts in the third period are due to that the prominence erupts toward the observer. We suggest that the faint component appears due to the decreasing of the plasma density, and the latter results from the expansion of the prominence spine.
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spelling doaj.art-f15a9ea4ff6a4be09f068096738f6a052022-12-21T18:29:39ZengFrontiers Media S.A.Frontiers in Physics2296-424X2021-09-01910.3389/fphy.2021.750097750097Spectral Evolution of an Eruptive Polar Crown Prominence With IRIS ObservationsJianchao Xue 0Hui Li 1Hui Li 2Yang Su 3Yang Su 4Key Laboratory of Dark Matter and Space Astronomy, Purple Mountain Observatory, Chinese Academy of Sciences, Nanjing, ChinaKey Laboratory of Dark Matter and Space Astronomy, Purple Mountain Observatory, Chinese Academy of Sciences, Nanjing, ChinaSchool of Astronomy and Space Science, University of Science and Technology of China, Hefei, ChinaKey Laboratory of Dark Matter and Space Astronomy, Purple Mountain Observatory, Chinese Academy of Sciences, Nanjing, ChinaSchool of Astronomy and Space Science, University of Science and Technology of China, Hefei, ChinaProminence eruption is closely related to coronal mass ejections and is an important topic in solar physics. Spectroscopic observation is an effective way to explore the plasma properties, but the spectral observations of eruptive prominences are rare. In this paper we will introduce an eruptive polar crown prominence with spectral observations from the Interface Region Imaging Spectrograph (IRIS), and try to explain some phenomena that are rarely reported in previous works. The eruptive prominence experiences a slow-rise and fast-rise phase, while the line-of-sight motions of the prominence plasma could be divided into three periods: 2 hours before the fast-rise phase, opposite Doppler shifts are found at the two sides of the prominence axis; then, red shifts dominate the prominence gradually; in the fast-rise phase, the prominence gets to be blue-shifted. During the second period, a faint component appears in Mg ii k window with a narrow line width and a large red shift. A faint region is also found in AIA 304Å images along the prominence spine, and the faint region gets darker during the expansion of the spine. We propose that the opposite Doppler shifts in the first period is a feature of the polar crown prominence that we studied. The red shifts in the second period are possibly due to mass drainage during the elevation of the prominence spine, which could accelerate the eruption in return. The blue shifts in the third period are due to that the prominence erupts toward the observer. We suggest that the faint component appears due to the decreasing of the plasma density, and the latter results from the expansion of the prominence spine.https://www.frontiersin.org/articles/10.3389/fphy.2021.750097/fullSun: coronaSun: coronal mass ejections (CMEs)Sun: filamentsprominencesSun: UV radiationtechniques: spectroscopic
spellingShingle Jianchao Xue 
Hui Li 
Hui Li 
Yang Su 
Yang Su 
Spectral Evolution of an Eruptive Polar Crown Prominence With IRIS Observations
Frontiers in Physics
Sun: corona
Sun: coronal mass ejections (CMEs)
Sun: filaments
prominences
Sun: UV radiation
techniques: spectroscopic
title Spectral Evolution of an Eruptive Polar Crown Prominence With IRIS Observations
title_full Spectral Evolution of an Eruptive Polar Crown Prominence With IRIS Observations
title_fullStr Spectral Evolution of an Eruptive Polar Crown Prominence With IRIS Observations
title_full_unstemmed Spectral Evolution of an Eruptive Polar Crown Prominence With IRIS Observations
title_short Spectral Evolution of an Eruptive Polar Crown Prominence With IRIS Observations
title_sort spectral evolution of an eruptive polar crown prominence with iris observations
topic Sun: corona
Sun: coronal mass ejections (CMEs)
Sun: filaments
prominences
Sun: UV radiation
techniques: spectroscopic
url https://www.frontiersin.org/articles/10.3389/fphy.2021.750097/full
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