Journal cover Journal topic
Annales Geophysicae An interactive open-access journal of the European Geosciences Union
Journal topic
Ann. Geophys., 37, 765–773, 2019
https://doi.org/10.5194/angeo-37-765-2019

Special issue: Solar magnetism from interior to corona and beyond

Ann. Geophys., 37, 765–773, 2019
https://doi.org/10.5194/angeo-37-765-2019

Regular paper 30 Aug 2019

Regular paper | 30 Aug 2019

# Signatures of red-shifted foot points in the quiescent coronal loop system

Signatures of red-shifted foot points in the quiescent coronal loop system
Yamini K. Rao1, Abhishek K. Srivastava1, Pradeep Kayshap2, and Bhola N. Dwivedi1 Yamini K. Rao et al.
• 1Department of Physics, Indian Institute of Technology (BHU), Varanasi 221005, India
• 2Institute of Physics, University of South Bohemia, Branišovská 1760, 370 05 České Budějovice, Czech Republic

Correspondence: Abhishek K. Srivastava (asrivastava.app@itbhu.ac.in)

Abstract

We observed quiescent coronal loops using multi-wavelength observations from the Atmospheric Imaging Assembly (AIA) aboard the Solar Dynamics Observatory (SDO) on 13 April 2016. The flows at the foot points of such loop systems are studied using spectral data from the Interface Region Imaging Spectrograph (IRIS). The Doppler velocity distributions at the foot points lying in the moss region show the negligible or small flows at the Ni I, Mg II k3, and C II line corresponding to upper photospheric and chromospheric emissions. Significant red shifts (downflows) ranging from 1 to 7 km s−1 are observed at Si IV (1393.78 Å; $\mathrm{log}\left(T/K\right)=\mathrm{4.8}$), which is found to be consistent with the existing results regarding dynamical loop systems and moss regions. Such downflows agree well with the impulsive heating mechanism reported earlier.

1 Introduction

The active regions dominated by various loop structures are of significant importance for the study of coronal heating, since these loop systems act as a fundamental unit of the solar corona . Moss is generally associated with plage regions around the active regions , and transition region (TR) emission of hot core loops will provide us with a better understanding of the flows and thus the energy-transfer mechanism between the TR and corona.

provided a full review of the coronal heating problem. It describes how the coronal heating mechanisms are impulsive when explored from the perspective of elemental magnetic flux strands. It has also been well established that the loop structures emit significantly in the solar corona, which has been classified depending on their temperatures. The spectral studies of these loop systems in response to the Doppler shift provide a clue for distinguishing between the steady and impulsive heating mechanism .

Various types of loops are hot core loops , warm loops , fan loops (Young et al.2012; Warren and Brooks2009, and references therein), and cool loops present in the different regions of the solar atmosphere. The temperature and density diagnostics of quiescent coronal loops have been studied earlier to some extent . However, there have not been many observations regarding the flows in the resolved strands or flux tubes of such loops in the solar corona.

Figure 1Intensity emission due to 171 Å wavelength of SDO–AIA at 19:13:22 UT. The yellow box is overlaid to show the region of interest (ROI) taken to analyze the flows at the foot points of quiescent coronal loops.

Figure 2Mosaic representation of the zoomed-in view of the region of interest at different wavelengths of SDO–AIA, as mentioned in the corresponding panels.

In this paper, we study quiescent coronal loops with big loop arches that have one of their foot points anchored at the edges of moss region. The different strands in such large loop systems were identified using high-resolution observations of SDO–AIA (Solar Dynamics Observatory – Atmospheric Imaging Assembly), and the flows in it were studied, mapping the foot points to the lower region of the solar atmosphere. Section 2 describes the observational data and their analyses, presenting the details of the data used for our analyses. In Sect. 3, the results have been reported with their interpretations. In the last section, the discussions and conclusions are summarized.

Figure 3(a) HMI map indicating the magnetic polarities at the moss region, indicted by blue contours. (b) Identification of the foot points of quiescent loops anchored at the moss regions. The different small boxes that are taken at the foot points of the individual loop strands are shown in both the panels.

Figure 4Differential emission measure maps of the plage region containing the moss associated to foot points of quiescent coronal loop systems.

2 Observational data

The Interface Region Imaging Spectrograph (IRIS) provides spectral data in the two UV domains: the FUV band (1331.7 to 1358.4 Å and 1389.0 to 1407.0 Å) and NUV band (2782.7 to 2835.1 Å), with a large number of spectral lines covering the photosphere, chromosphere, TR, and inner corona. Level 2 data are used for our study which are calibrated for the dark current removal and flat fielding effect . We utilized Si IV (1393.78 Å), Mg II k (2796.20 Å), C II (1334.53 Å), and Ni I (2799.47 Å) spectral lines.

Figure 5The different parametric plots of Si IV (1393.78 Å) line, with the foot points of the quiescent coronal loop systems being indicated by different boxes. DN refers to the data number.

Figure 6The velocity distributions for different spectral lines corresponding to different temperatures at box B1.

In our present work, we used dense raster data from IRIS for the time period 19:19:09 to 20:21:14 UTC on 13 April 2016, targeting the evolution of AR 12529 with a slit width of 0.35 in and a step cadence of 9.3 s, covering the field of view of 141′′ in the x direction and 175 in in the y direction and centered at the coordinates (${X}_{\mathrm{cen}},{Y}_{\mathrm{cen}}\right)=$4 (-173 in, 275 in). The data are compensated for oscillations due to thermal variation using iris_orbitvarr_corr_l2.pro in the SSWIDL library. The rest wavelengths for different spectral lines used in our analysis are calibrated using neutral lines from the relatively quiet-Sun area of the raster. The rest wavelength of Ni I used is 2944.4697 Å. Mg II k was calibrated with respect to Ni I, which is found to be 2796.3574 Å. The Si IV line is calibrated with respect to the Fe I (1392.8052 Å) line, and C II is calibrated with respect to O I (1355.5987 Å). Thus, the calibrated wavelengths used for our analysis are 1393.7604 and 1334.5406 Å for Si IV and C II respectively.

The Doppler velocities are deduced using different spectral lines, i.e., Ni I 2799.47 Å, Mg II k 2796.20 Å, C II 1334.53 Å, and Si IV 1393.78 Å, respectively associated with the formation temperature of $\mathrm{log}\left(T/K\right)=\mathrm{4.2}$, 4.0, 4.3, and 4.8. The velocity resolution of IRIS is 1 km s−1 .

Si IV shows the characteristics of an optically thin line and is thus fitted with the single Gaussian curve, while Ni I is the absorption line and the inverse Gaussian curve is fitted. Mg II k and C II are fitted with single or double Gaussian, depending on their profile characteristics.

The corresponding SDO–AIA observations are also taken in the different filters covering the UV–EUV range, corresponding to a different temperature range in the solar atmosphere. AIA provides full-disk multi-wavelength observations of coronal lines, with a spatial resolution of 1.5 in, a pixel size of 0.6 in, and a temporal cadence of 12 s .

The co-aligned Level 2 SDO–AIA data cube was used in which all the wavelengths are matched to the field of view of 1600 Å. To co-align with the raster images of Si IV (1393.78 Å), the near-time 171 Å image properly cross-correlated with 1600 Å was used to compensate for the different resolution of two instruments. However, in our paper, we study the bulk plasma flows from the chosen moss region (in various boxes) by deducing the integrated spectral line profiles of various IRIS lines. The plage regions are identified in SDO–AIA image data, and the location is mapped onto comparatively high-resolution IRIS data.

Figure 7The velocity distributions for different spectral lines corresponding to different temperatures at box B2.

Figure 8The velocity distributions for different spectral lines corresponding to different temperatures at box B3.

3 Observational results

Figure 1 shows the intensity emission of AR 12529, where the plage region and various loops anchored in the moss region are visible in the 171 Å wavelength of SDO–AIA. The green emission predominantly indicates the highest emission representing the part of the moss region. The yellow box is overlaid to show the region of interest (ROI).

In Fig. 2, the moss region has been identified with the brightest emission in the SDO–AIA 193 Å filter. The intensity threshold of above 3000 counts (see Fig. 1), with values double those of the plage region surrounding it, was set, which is shown by contours overlaid over the different filters, corresponding to different temperature ranges from the upper photosphere to the corona. The northern segment of the moss regions where the quiescent coronal loops are anchored was further taken to analyze the flows at the foot points of these loop systems. The different bands of AIA show different morphological characteristics of an AR; 1600 and 1700 Å represent the continuum emission at the upper photosphere, showing the plage region near the active region, and 304 Å yields the chromospheric emission of the plage region. The hot loop structures are not distinctly visible. The middle row shows the inner coronal channels where quiescent coronal loops are clearly visible, and the moss region is identified. The last row shows the hot channels of SDO–AIA (335, 211, and 94 Å) where the quiescent loops taken for our analysis are not visible, since quiescent loops are dominated by emissions from the temperatures ranging from 0.7 to 1 MK, corresponding to SDO–AIA filters.

Figure 3a shows the line-of-sight magnetogram of the region of interest (ROI) taken from the Helioseismic Magnetic Imager (HMI) aboard SDO (HMI/SDO), indicating the magnetic polarities at the moss region as well as foot points of the quiescent coronal loops. Figure 3b is the emission of the 193 Å line, plotted in reverse color to identify the foot points. The different boxes of different sizes are then chosen around the foot points to cover the full strand of loop.

Figure 5 shows the parametric plots of the Si IV (1393.7604 Å), showing the intensity, Doppler velocity, and FWHM (full width at half maximum) maps where the values are indicated by the color bars over the plots. The Doppler velocity maps show that the TR is dominated by red shifts even in the plage region surrounding the moss in which foot points were taken for our analysis.

Figure 4 shows the differential emission measure (DEM) maps of the ROI, derived by using the automated method discussed by in which plasma emission at different temperatures is shown. The color bar indicates the range of the DEM values. These maps show the presence of multi-thermal plasma at the foot points of the quiescent coronal loop systems shown by the boxes around it.

Figure 9The velocity distributions for different spectral lines corresponding to different temperatures at box B4.

Figure 10The velocity distributions for different spectral lines corresponding to different temperatures at box B5.

The Doppler velocity distribution is thus explored at different locations, labeled as B1, B2, B3, B4, and B5. Positive values (red shifts) represent downflows, while the negative values (blue shifts) indicate upflows. The Doppler velocity at each pixel in first box (B1) for different spectral lines is then shown in Fig. 6. The velocity distribution for Ni I shows the spread around 0 km s−1, ranging from −0.8 to +2.2km s−1. Mg II k shows the velocities, ranging from −5 to +1km s−1, while C II ranges from −5 to +5km s−1. Si IV shows red shifts with Doppler velocities ranging from 0 to +15km s−1. The histogram of the Doppler velocity for different spectral lines indicates the red shifts in the Si IV line and very small or negligible flows at Ni I, Mg II k, and C II.

Similarly, such Doppler velocity distribution is shown in Figs. 7, 8, 9, and 10 for different boxes, labeled as B2, B3, B4, and B5.

Figure 11 shows the average Doppler shift of different spectral lines as a function of their temperatures for different boxes chosen at the foot points of the loops. Ni I (2799.47 Å) corresponds to the upper photosphere, and Mg II k yields emission ranging from the mid-chromosphere to upper chromosphere. The core defined by (k3) forms little higher than the wings at 200 km below TR . The C II core yields emission from 2.1 Mm, while Si IV corresponds to the TR emission .

The Doppler velocity of the Ni I line has negligible values, indicating almost no flows (0.27 to 0.70 km s−1), corresponding to the photospheric region. The blue shifts (upflows) show small increments for B2, B4, and B4 (−0.11 to −0.31km s−1), while they remain almost the same for B1 (0.16 km s−1) and B5 (0.80 km s−1) up to the formation temperature of Mg II k. The C II line shows considerable blue shifts (upflows) of −0.17 to −2.81km s−1, but it is still negligible when compared to chromospheric flows. The Doppler velocity variation at Si IV shows prevalent red shifts (downflows) at all the locations corresponding to TR flows (0.37 to 6.97 km s−1). The 1σ error is shown as error bars, which is difficult to visualize in Fig. 11, owing to its very small values.

Figure 11Average Doppler velocity variations for different spectral lines dominating at different heights in the solar atmosphere for boxes B1, B2, B3, B4, and B5 at the foot points of quiescent coronal loops.

4 Discussions and conclusions

The co-spatial multi-spectral Doppler velocity trend at the foot points of quiescent coronal loops was studied. The Doppler velocity variation shows small flows (upflows and downflows) for Ni I and Mg II k in the photospheric as well as the chromospheric region. C II shows very blue shifts (−0.1 to −2.81km s−1), indicating small upflows at the upper chromospheric region. The Doppler velocities then change to red shifts at the formation temperature of the Si IV line, corresponding to the TR.

It was previously shown that the moss regions show significant red shifts (downflows) in the TR, explaining the low-frequency heating . The high- and low-frequency mechanisms depend on the time taken by the loops to cool down when compared to heating frequency .

Our study of the flows at the quiescent coronal loops shows similar characteristics to the dynamically active loops, though the velocity values are smaller. The plasma predominantly shows red shifts at TR temperatures which corroborate with the low-frequency heating of loops in the coronal part of the solar atmosphere. These observations thus agree with the coronal loops heated up by low-frequency nanoflares via an impulsive heating mechanism. Also, observed the symmetric profiles for steady heating in the loops. Though it is possible to have asymmetries in the individual profile for which velocity distribution has been observed, our speculation supports the nanoflare-driven impulsive heating mechanism for the quiescent coronal loops.

The asymmetries may also cause the Doppler variation in the spectral profiles due to a difference in the pressures. . Thus, other possibilities cannot be ruled out.

Data availability
Data availability.

All the data which we have used in the paper can be accessed publicly at http://www.iris.lmsal.com/search/ (last access: 19 July 2019).

Author contributions
Author contributions.

All authors have contributed in an equal manner.

Competing interests
Competing interests.

The authors declare that they have no conflict of interest.

Special issue statement
Special issue statement.

This article is part of the special issue “Solar magnetism from interior to corona and beyond”. It is a result of the Dynamic Sun II: Solar Magnetism from Interior to Corona, Siem Reap, Angkor Wat, Cambodia, 12–16 February 2018.

Acknowledgements
Acknowledgements.

We acknowledge the use of IRIS observations. IRIS is a NASA Small Explorer mission developed and operated by the Lockheed Martin Solar and Astrophysics Laboratory (LMSAL), with mission operations executed at the NASA Ames Research Center and major contributions to downlink communications funded by the Norwegian Space Centre (NSC; Norway) through an ESA PRODEX contract.

Financial support
Financial support.

Yamini K. Rao is fully supported by the financial grant from the ISRO RESPOND project.

Review statement
Review statement.

This paper was edited by Viktor Fedun and reviewed by two anonymous referees.

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