The following article is Open access

Sun-as-a-star Spectroscopic Observations of the Line-of-sight Velocity of a Solar Eruption on 2021 October 28

, , , , , and

Published 2022 May 26 © 2022. The Author(s). Published by the American Astronomical Society.
, , Citation Yu Xu et al 2022 ApJ 931 76 DOI 10.3847/1538-4357/ac69d5

Download Article PDF
DownloadArticle ePub

You need an eReader or compatible software to experience the benefits of the ePub3 file format.

0004-637X/931/2/76

Abstract

The propagation direction and true velocity of a solar coronal mass ejection, which are among the most decisive factors for its geo-effectiveness, are difficult to determine through single-perspective imaging observations. Here we show that Sun-as-a-star spectroscopic observations, together with imaging observations, could allow us to solve this problem. Using observations of the Extreme Ultraviolet Variability Experiment onboard the Solar Dynamics Observatory, we found clear blueshifted secondary emission components in extreme-ultraviolet spectral lines during a solar eruption on 2021 October 28. From simultaneous imaging observations, we found that the secondary components are caused by a mass ejection from the flare site. We estimated the line-of-sight (LOS) velocity of the ejecta from both the double Gaussian fitting method and the red-blue asymmetry analysis. The results of both methods agree well with each other, giving an average LOS velocity of the plasma of ∼423 km s−1. From the 304 Å image series taken by the Extreme ultraviolet Imager onboard the Solar Terrestrial Relation Observatory-A (STEREO-A) spacecraft, we estimated the plane-of-sky velocity from the STEREO-A viewpoint to be around 587 km s−1. The full velocity of the bulk motion of the ejecta was then computed by combining the imaging and spectroscopic observations, which turns out to be around 596 km s−1 with an angle of 42fdg4 to the west of the Sun–Earth line and 16fdg0 south to the ecliptic plane.

Export citation and abstract BibTeX RIS

Original content from this work may be used under the terms of the Creative Commons Attribution 4.0 licence. Any further distribution of this work must maintain attribution to the author(s) and the title of the work, journal citation and DOI.

1. Introduction

Coronal mass ejections (CMEs) are the largest-scale eruptive events on the Sun. Interaction of CMEs with the Earth's magnetosphere could cause geomagnetic storms, which may pose major threats to man-made satellites and astronauts (Gonzalez et al. 1994; Echer et al. 2008). The propagation direction and true velocity are among the key factors that affect the geo-effectiveness of a CME (Moon et al. 2005; Kim et al. 2008), and thus their accurate determination is of great importance.

One way to obtain the true velocity of a CME is to combine its plane-of-sky (POS) velocity and its line-of-sight (LOS) velocity. The POS velocities of CMEs are often obtained from imaging observations with coronagraphs or extreme-ultraviolet (EUV) imagers. The motion of ejected materials along the LOS toward observers can cause, according to the Doppler effect, blueshifts or blueshifted components in spectral line profiles (e.g., Tian et al. 2012, 2013), through which one can calculate the LOS velocities of the ejecta. Thus, combining the POS and the LOS velocities, one can obtain the true velocities and propagation directions of CMEs. For example, Susino et al. (2013) studied a CME associated with a filament eruption and calculated the true velocities of both the CME front and the CME core. The POS velocities were obtained from images taken by the Large Angle and Spectrometric COronagraph (Brueckner et al. 1995) onboard the Solar and Heliospheric Observatory (SOHO) while the LOS velocities were computed using the blueshifted component in O vi 103.2 nm Å line profiles observed by the slit spectrometer Ultraviolet Coronagraph Spectrometer (Kohl et al. 1995) onboard SOHO. The true velocities of the CME front and core were then computed using the geometric relationship, which turned out to be ∼578 km s−1 and ∼583 km s−1, respectively.

Apart from estimating true velocities using the LOS and POS velocities, another method for reconstructing the three-dimensional (3D) propagation track of a CME is using multiviewpoint observations. The twin Solar Terrestrial Relation Observatory (STEREO; Kaiser et al. 2008) satellites provide view angles off the Sun–Earth line and offer opportunities for 3D reconstructions of CME tracks through multiple-viewpoint observations. Several 3D reconstruction techniques were developed, such as the tie-pointing method (e.g., Inhester 2006; Thompson 2009; Liewer et al. 2011), the polarization ratio technique (Moran & Davila 2004), and the mask-fitting method (Feng et al. 2012, 2013; Ying et al. 2022). Mishra & Srivastava (2013) estimated the true velocity of a CME using the data from COR2 in the Sun Earth Connection Coronal and Heliospheric Investigation (SECCHI; Howard et al. 2008), and predicted the arrival time of that CME by assuming that the velocity remains constant beyond the field of view (FOV) of the COR2. Susino et al. (2014) tracked the position and velocity variation of an erupting filament using the image series from the Extreme Ultraviolet Imager (EUVI; Wuelser et al. 2004) based on the tie-pointing technique. They also reconstructed the 3D shape of the CME front from the polarization ratio method using the observations from SECCHI/COR1. By combining both the tie-point method and a supervised computer vision algorithm, Braga et al. (2017) obtained the velocity vectors of 17 CME events using the imaging observations from the twin STEREO spacecraft.

The restriction of the first method (i.e., combining the POS and LOS velocities) in estimating true velocities mainly comes from the limited FOV of a slit spectrometer, which significantly lowers the opportunity to capture CMEs. Also, this method can only be conducted when the slit covers the CME area during its early expansion. The second method (i.e., using multiviewpoint observations) relies on observations from multiple viewpoints, which requires appropriate positions of different spacecraft to ensure simultaneous detection of the same single CME. This requirement often means a large increase in the cost of the whole mission. A low-cost Sun-as-a-star spectrograph that measures the full-disk integrated EUV spectra, which is similar to that in stellar observations, could overcome such drawbacks, as it is able to catch almost all CMEs originating from the front side of the solar disk and provide continuous monitoring of the early propagation of CMEs (Yang et al. 2022). Moreover, such observations could provide a unique reference for us to understand CMEs on other stars, whose signals can only be extracted from point-source spectra at present.

Current Sun-as-a-star spectral observations are conducted by the Extreme ultraviolet Variability Experiment (EVE; Woods et al. 2012) onboard the Solar Dynamic Observatory (SDO; Pesnell et al. 2012). The Doppler shifts in spectra observed by EVE are still insufficiently investigated. Previous studies have revealed shifts of spectral line centroids during solar flares. For instance, Hudson et al. (2011) analyzed the EVE spectra during a flare and found redshifts around 17 km s−1 in the He ii 30.4 nm line as well as decreasing blueshifts in the Fe xxiv 19.2 nm line, which were interpreted as signatures of chromospheric evaporation. Brown et al. (2016) studied the Doppler shifts in hydrogen Lyman lines in six flares, calculated the Doppler velocities using three different methods, and found that both redshifts and blueshifts in those Lyman lines were around 10 km s−1. They attributed the blueshifts in the low-temperature chromospheric lines to (1) the upflows of a cool, neutral hydrogen layer pushed upwards due to the heating in the deep chromosphere and (2) ejecta captured by the Atmospheric Imaging Assembly (AIA; Lemen et al. 2012) onboard SDO. Chamberlin (2016) investigated the shifts of the line centroids caused by instrumental effects and presented the optical correction function of wavelengths for the He ii 30.4 nm line. They also conducted a study of the X1.8 flare with a streamer blowout observed by SDO/AIA in the 304 Å passband on 2011 September 7. The peak Doppler velocity of the He ii 30.4 nm line calculated from the optically corrected spectra turned out to be ∼120 km s−1. Cheng et al. (2019) studied various types of plasma motions in two flare regions using spectra from EVE. Their single Gaussian fitting revealed blueshifts in the high-temperature lines and redshifts in the relatively cool lines in the flare's gradual phase. They suggested that the blueshifts represent plasma upflows caused by chromospheric evaporation while the redshifts result from loop contraction or chromospheric condensation.

It is worth mentioning that a spectral line profile at the location of a solar eruption generally should consist of at least two components—a component from the nearly stationary background emission and the other one from the moving plasma (e.g., Tian et al. 2012). In the full-disk integrated spectra, the background component is normally much stronger. If the spectral resolution is too low, the total spectral profile may reveal a slight enhancement at the line wing or appear to be slightly shifted. In previous Sun-as-a-star spectroscopic investigations, a single Gaussian fitting was often used to reveal the Doppler shift of an entire line profile, which should be smaller than the true speed of the moving plasma (e.g., Tian et al. 2011). The blueshifted secondary components caused by plasma motions along the LOS toward observers in the Sun-as-a-star spectra have not been detected yet.

With recent EVE observations, we identified the blueshifted secondary components in full-disk integrated spectra caused by a mass ejection and calculated the LOS velocity of the ejecta. We combined this with the POS velocity from the STEREO-A viewpoint to obtain the full velocity (i.e., true velocity) of the bulk motion of the ejected plasma. Section 2 gives a brief introduction to the observations from SDO/EVE and STEREO-A/EUVI. Section 3 presents the data analysis results and relevant discussions. Finally, we summarize our finding in Section 4.

2. Observations

The EVE onboard SDO is a full-disk integrated spectrometer measuring the solar EUV irradiance from 6 nm to 106 nm with a spectral resolution of ∼0.1 nm and a time cadence of ∼10 s. The sampling wavelength interval is 0.02 nm, which enables detection of Doppler velocities at tens of kilometers per second (Hudson et al. 2011). The Multiple EUV Grating Spectrographs-A (MEGS-A) included in EVE experienced an anomaly on 2014 May 26, and after that no spectra at wavelengths shorter than 33 nm are available. The integration time for MEGS-B was then adjusted to 1 minute for a higher signal-to-noise ratio.

The target mass ejection occurred on October 28, after an X1.0 flare in AR 12887. The flare's onset is at 15:24 UT and the X-ray flux in 1–8 Å measured by GOES-16 reaches its peak at 15:32 UT (see Figure 1(a)). A filament in the active region (AR) rises and appears to be heated to higher temperatures, becoming a bright structure in AIA 304 Å that erupts during the flare's impulsive phase. It is then followed by another sympathetic filament eruption at around 15:35 UT, which is located at the east footpoint of the aforementioned filament. This event generates a global EUV wave, which was recently analyzed by Hou et al. (2022). In Figure 1(b), the 304 Å image taken by SDO/AIA shows the location of the source AR (i.e., AR 12887) and that of the first filament whose rising and heating leads to the target ejection.

Figure 1.

Figure 1. (a) The relative flux in 1–8 Å from GOES. The red vertical dashed lines indicate the flare's onset and peak at 15:24 UT and 15:32 UT, respectively. The blue line shows the quiescent level of X-ray flux. (b) The AIA 304 Å image before the flare's onset. The green arrow shows the location of the first filament.

Standard image High-resolution image

In the meantime, STEREO-A/EUVI captured the eruption at around 37fdg5 east to the Sun–Earth line (see Figures 2(b)–(c)), and the positions of STEREO-A and the Earth are shown in Figure 2(a) under the Heliocentric Earth Ecliptic (HEE) coordinate system. The x-axis of the HEE system points from the center of the Sun toward the Earth and the z-axis points along the ecliptic north pole (Thompson 2006). The STEREO-A/EUVI images the Sun in four channels (i.e., 30.4, 17.1, 19.5, and 28.4 nm) spanning the 0.1–20 MK temperature range. We used the image series of 30.4 nm for velocity analysis (see Section 3.1). The time interval between two adjacent 30.4 nm images is 2.5 minutes.

Figure 2.

Figure 2. (a) The positions of STEREO-A and the Earth at 15:30 UT on 2021 October 28 in the HEE coordinate system. (b) The ejecta observed by STEREO-A in the 304 Å passband at 15:28:15 UT. The blue dashed line outlines the bright ejecta. (c) The ejecta observed by STEREO-A in the 304 Å passband at 15:33:15 UT. The gray dashed lines are the cuts chosen for the time-space analysis (see the text in Section 3.1) and the numbers at the end of the dashed lines label the cuts. (d) The time-distance diagrams for Cut 2, Cut 3, Cut 5, and Cut 7 (see Section 3.1 for more details).

Standard image High-resolution image

3. Analysis and Results

3.1. Velocity Estimation from STEREO Observations

We derived the POS (from the STEREO-A viewpoint) velocity of the ejecta using a series of 304 Å images from STEREO-A observations. The EUVI images were rectified using secchi_prep.pro in the SolarSoftWare 4 package with the keyword rotated_on applied to rotate the solar north up in the images. We chose eight cuts (gray dashed lines in Figure 2(c)) along the directions of plasma motion. Then we derived the speeds of the ejecta along the eight directions from time-distance diagrams. The measurements are under the helioprojective-Cartesian (HPC) coordinate system in EUVI images. The HPC system owns a z-axis along the Sun-observer line and y-axis perpendicular to the z-axis in the plane containing both the solar north pole and the z-axis. The x-axis is perpendicular to both y-axis and z-axis, forming a right-handed coordinate system (see Thompson 2006 for more details).

No obvious acceleration was seen in the time-distance diagrams (Figure 2(d)), which can be attributed to the poor time cadence of EUVI as the initial acceleration process of the mass eruption was completed within 2 minutes. We then reasonably assumed that the ejecta moved along each cut at a constant speed. At each time step between 15:20 UT and 15:50 UT along each cut, the location of the moving plasma front was identified as the position where the intensity reaches its maximum value. For each cut, locations of the fronts form a track of the ejecta and we applied a linear fitting to the track to estimate the speed. The average velocity of the ejecta vPOS and its angle with respect to the +x-axis direction of the HPC system (i.e., Solar X in Figures 2(b)–(c)) were then computed using the following equations,

Equation (1)

Equation (2)

where vi and θi are the speed along Cut i (i = 1, 2,..,8) and the angle between the +x-axis direction of the HPC system and the direction of Cut i, respectively. All angles are measured counterclockwise with respect to the +x-axis direction of the HPC system. Pi is the Pearson correlation coefficient that indicates the linear correlation between the front locations and the corresponding times. The identification of the ejecta fronts by maximum intensity values in the time-distance diagrams occasionally results in nonlinearity in the track of the ejecta, so we used Pi as weighting factors in Equations (1)–(2). The average POS velocity turned out to be around 587 km s−1 with an angle of around −17fdg8 to the +x-axis direction of the HPC system.

3.2. EVE Observations of Spectral Line Intensities

We chose the spectra observed by SDO/EVE MEGS-B from 11:00 UT to 21:00 UT for analysis. First, we selected six spectral lines (listed in Table 1) for detailed analysis and checked line blends for each of them using the CHIANTI 10.0.1 (Dere et al. 1997; Del Zanna et al. 2021) database. Lines listed in Table 1 do not have obvious blends except for a red wing blend in Ne vii 46.52 nm with Ca ix 46.63 nm. Second, we calculated the intensity variation with time for each line. We applied a single Gaussian fitting (linear background for the continuum) to all the lines in Table 1 at each time step and obtained their line intensities. We defined a quiescent time, which was chosen to start from 11:00 UT to 13:00 UT when no obvious flare is observed (except for a small C2.2 flare at around 12:26 UT). The quiescent intensity level for each line was obtained by averaging the line intensities over the quiescent time period. The intensity variations for each line relative to their quiescent levels are displayed in Figure 3. The pre-flare relative intensities of all lines maintain a level around one, which validates the choice of the quiescent time to be reasonable. The intensities of all lines begin to rise right after the flare's onset. The lines formed below 105.8 K reach their peaks before the flare's peak, and the Ne viii 77.03 nm line with a formation temperature above 105.8 K reaches its peak around the time of the GOES soft X-ray peak. We noticed that almost all the spectral lines show dimming signatures (i.e., intensity dropping below the quiescent level) during and after the flare's gradual phase except for O iii 52.57 nm. We roughly quantified the dimming depth by averaging the decrease of the relative intensity from 19:00 UT to 21:00 UT when the flare almost ends. The dimming depths are marked in Figure 3, with positive values indicating dimming while negative enhancement. We suggest that the dimming is caused by the loss of plasma due to the mass ejection, in which the decrease of plasma density in the source region leads to the decrease of EUV emission. Signatures of CME-induced dimmings have been identified from EVE observations (e.g., Mason et al. 2014, 2016; Harra et al. 2016). In these previous observations, the dimmed lines usually have a minimum formation temperature of ∼105.8 K. Here we show that the dimming also exists in relatively cooler lines such as He i 58.43 nm, O v 62.96 nm, and O vi 103.1 nm, which suggests that some plasma in the lower atmosphere rises and erupts, resulting in the mass-loss dimming.

Figure 3.

Figure 3. The relative intensity variations for the selected spectral lines. The red vertical dashed lines indicate the flare's onset and peak at 15:24 UT and 15:32 UT, respectively. The solid blue line represents the quiescent intensity level. The average dimming depth during 19:00 UT to 21:00 UT for each line is marked in each panel (positive for dimming while negative for enhancement).

Standard image High-resolution image

Table 1. Spectral Lines Selected for Analysis in EVE MEGS-B Dataset

IonRest Wavelength a (nm)log (T/K)
He i 58.43034.16
O iii 52.57704.92
O v 62.96835.37
O vi 103.1915.47
Ne vii b 46.52205.71
Ne viii 77.03655.81

Notes.

a The rest wavelengths were obtained by averaging the centroid locations of line profiles observed during the quiescent time (see the text for details). b The red wing of Ne vii 46.52 nm is contaminated by Ca IX 46.63 nm.

Download table as:  ASCIITypeset image

3.3. EVE Observations of the LOS Velocities

We examined the line profile variations for each line and identified emission enhancement in the blue wing during the impulsive phase and after the flare's peak. For each spectral line, we obtained a reference line profile by averaging the line profiles during the quiescent time, and then subtracted the reference line profile from the observed line profiles to obtain the pre-flare subtracted line profiles. Temporal evolutions of the pre-flare subtracted line profiles of O iii 52.57 nm, O v 62.96 nm, and O vi 103.1 nm are displayed in Figure 4. In order to diminish the effect of the sympathetic filament eruption at around 15:35 UT (as described in Section 2), we only display the pre-flare subtraction analysis results from 15:23:30 UT to 15:34:30 UT. The wavelength λ was converted into the offset velocity vc through the following equation,

Equation (3)

where c = 2.9979 × 105 km s−1 is the light speed in the vacuum; λ0 is the rest wavelength of the line, which was computed by averaging the central wavelengths, obtained from the single Gaussian fitting during the quiescent time period. Figure 4 shows the enhancement peaks near the rest wavelength and in the blue wing at around 500 km s−1 in each of the spectral lines, which we suggested was caused by the outward movement of the heated plasma. The pre-flare subtraction was also conducted for the other three lines and the variations in He i 58.43 nm and Ne vii 46.52 nm are similar to those in the oxygen lines. The emission enhancements at the blue wings of those lines suggest that the heated filament contains plasma with a temperature range of about 0.02 MK–0.5 MK (i.e., the formation temperature of He i 58.43 nm; the formation temperature of Ne vii 46.52 nm). However, the variations in the Ne viii 77.03 nm line are much more fluctuated than the others and more than one peak was detected. The existence of fluctuation in the Ne viii 77.03 nm line still needs further investigation.

Figure 4.

Figure 4. (a) The pre-flare subtracted line profiles for O iii 52.57 nm, (b) O v 62.96 nm, and (c) O vi 103.1 nm from 15:23:30 UT to 15:34:30 UT. The observation times are labeled on the right side of each profile and the y-axis is offset for a better illustration. The gray dashed lines indicate the level of spectral irradiance during the quiescent time. The vertical black lines indicate the rest wavelengths. The negative offset velocities represent the blue wings while the positive, the red.

Standard image High-resolution image

In order to further investigate the LOS velocity of the moving plasma, we analyzed the observed spectral profiles of the six emission lines during the flare. We found obvious secondary components in the blue wings of O iii 52.57 nm, O v 62.96 nm, and Ne vii 46.52 nm during the impulsive phase and shortly after the flare's peak. The spectral profiles of these lines at a specific time (15:29:30 UT) are shown in Figure 5. The small bulges in the blue wings suggest the presence of secondary components. To the best of our knowledge, this is the first time that a distinct secondary emission component caused by a mass ejection is detected in the Sun-as-a-star spectra. Through a single Gaussian fitting, previous investigations of several flares (see, e.g., Hudson et al. 2011; Brown et al. 2016; Chamberlin 2016; Cheng et al. 2019) all found shifts of line centroids that are mostly smaller than 100 km s−1. In these observations, no obvious secondary components were seen. The obvious bulges in the blue wings of the spectral lines (as shown in Figure 5) facilitate the conduction of double Gaussian fitting to derive the LOS speed of the ejecta.

Figure 5.

Figure 5. (a) Line profiles of O iii 52.57 nm, (b) O v 62.96 nm, and (c) Ne vii 46.52 nm observed at 15:29:30 UT, which are the results of double Gaussian fitting. The stars are the observed spectral irradiances while the error bars are derived from the measurement precision contained in the EVE observation files. The red dashed lines are the results of the double Gaussian fitting, and the gray curves represent the primary component while the blue, the secondary. The vertical lines indicate the locations of the center of the primary (gray) and that of the secondary (blue) components. The Doppler velocities derived from the double Gaussian fitting are labeled as v1 and v2 for the primary and secondary components, respectively.

Standard image High-resolution image

We conducted the double Gaussian fitting for line profiles of O iii 52.57 nm, O v 62.96 nm, and Ne vii 46.52 nm observed during the impulsive phase and several minutes after the flare's peak. We adopted the following expression for the double Gaussian fitting:

Equation (4)

where b0 was a constant background representing the continuum; in and λn (n = 1, 2) were the line peak intensity and central wavelength of the nth component, respectively. We followed the definition of exponential width in Tian et al. (2012) and used wn (n = 1, 2) to represent the exponential width (width hereafter) of the nth component. We regarded the primary component as the first component, which is located near the rest wavelength and represents emission from the background solar atmosphere. The secondary (or second) component is located in the blue wing of the line, which results from the outward moving ejecta. We adopted the double Gaussian fitting procedure used by Tian et al. (2011). The procedure requires initial guess values of centroids, widths, and peak intensities of the two Gaussian components and their variation ranges as inputs and iterates until a global minimization of the difference between the observed spectrum and the fitted one is reached. The initial values of the parameters were set as follows. We took the minimum spectral irradiance in an observed line profile as the initial constant background b0 and allowed it to vary from 75% to 125% of the initial value during the iterations. The initial central wavelengths of the primary and secondary components were set to be the rest wavelength and the wavelength corresponding to an offset velocity of −400 km s−1, respectively. The central wavelength of the primary component was allowed to vary from −20 km s−1 to 20 km s−1, a rough range of the shifts of line centroids derived from single Gaussian fitting found in previous EVE observations (Hudson et al. 2011; Brown et al. 2016). The centroid of the secondary component was allowed to vary within the blue wing. The initial peak intensity values of the primary and secondary components were set to be the spectral irradiances at the offset velocities of zero and −400 km s−1, respectively. The peak intensity of the primary component was allowed to vary within [75%, 125%] of the initial value, and that of the secondary component was allowed to vary from zero to the maximum spectral irradiance of the line profile. The initial widths of both components were set to equal the average width during the quiescent time, and their variation ranges during the iterations were [50%, 150%] and [50%, 125%] of the initial value, respectively. All the initial value settings were the results of trial and error. The uncertainty of the double Gaussian fitting coming from a large number of free parameters causes the failure of fitting, sometimes. We selected the valid fitting results based on the principle that the fitted profiles are located within the measurement error ranges of the observed profiles.

The double Gaussian fitting results at 15:29:30 UT for the three lines with obvious secondary components (i.e., O iii 52.57 nm, O v 62.96 nm, and Ne vii 46.52 nm) are shown in Figure 5, where we interpolated the wavelength points to make the fitted curves look much smoother. All three lines reveal a high-speed component with a velocity of 400–500 km s−1. The fitting results for O v 62.96 nm at different time steps are shown in Figure 6. The double Gaussian fitting failed in the first 2 minutes after the flare's onset, so we only show the results from 15:26:30 UT to 15:34:30 UT. Our analysis indicates that the plasma at around 0.2 MK (the formation temperature of the O v 62.96 nm line) moves at a speed around 400 km s−1 during the flare's impulsive phase and shortly after the flare's peak. The width of the primary component remains relatively constant, whereas that of the secondary component generally increases with time. This could be attributed to the expansion of the ejecta, which causes a wide velocity distribution and then results in a broadening of the line profiles. The variation of the peak intensity ratio of the two components shows that the secondary component reaches its peak at around 15:29:30 UT, which is ∼3 minutes before the flare's peak. The intensity ratio then gradually decreases. The velocities of the secondary components in all the three lines are plotted in Figure 8(a). We can see a slight increasing trend of the speeds from 15:26 UT to 15:30 UT in all the three lines, likely indicating the continuous acceleration process of the ejecta.

Figure 6.

Figure 6. The double Gaussian fitting results for O v 62.96 nm from 15:26:30 UT to 15:34:30 UT. The line styles, colors, stars, and error bars are the same as those in Figure 5. The Doppler velocity vn (n = 1, 2) and width wn (n = 1, 2) of the two components are labeled in each panel, where the gray (blue) represents the parameters of the primary (secondary) component. The peak intensity ratio of the primary component to the secondary component (i1/i2) is also shown in each panel.

Standard image High-resolution image

Another method for estimating the velocity of the secondary component is to use the red-blue (RB) asymmetry of the line profile (see, e.g., De Pontieu et al. 2009; Tian et al. 2011). The RB asymmetry profile (hereafter, RB profile) was calculated from the following equation

Equation (5)

where vc is the offset velocity computed using Equation (3) (here positive only) and δv is the velocity step in the RB profile calculation; I(v) is the observational or interpolated spectral irradiance around vc . The RB profile can be normalized to the peak intensity of the interpolated spectrum. From the peak of the RB(vc ) profile, we can infer parameters of the secondary component. We interpolated an observational line profile and adopted δv = 5 km s−1 to obtain the RB profile at each time step. We regarded the velocity where the RB profile peaks as the LOS velocity of the ejecta. Figure 7 shows the RB profile of the O v 62.96 nm line at 15:29:30 UT. The RB profile peaks at around 380 km s−1, which indicates a mass ejection moving toward Earth at the speed around 380 km s−1. Due to the blend at the red wing of Ne vii 46.52 nm, we only conducted an RB asymmetry analysis for the O iii 52.57 nm and O v 62.96 nm lines. The velocities of the secondary component derived from the RB analysis are shown in Figure 8(a).

Figure 7.

Figure 7. The RB profile of the line O v 62.96 nm at 15:29:30 UT. The green vertical dashed line indicates the velocity corresponding to the peak of the RB profile.

Standard image High-resolution image
Figure 8.

Figure 8. (a) LOS velocities calculated from the double Gaussian fitting method (stars) and from the RB asymmetry analysis (diamonds) for O iii 52.57 nm (yellow), O v 62.96 nm (green), and Ne vii 46.52 nm (pink). The vertical red dashed line indicates the time of the flare's peak. (b) A sketch of the full velocity calculation on the ecliptic plane for the mass ejection. (c) A snapshot of the full velocity calculation for the ejecta in 3D space. The yellow plane represents the ecliptic plane. The red/green/blue sphere shows the location of the Sun/Earth/STEREO-A. The arrows indicate the velocity vectors and the corresponding speed is labeled at the header of each arrow. A 3D interactive version of panel (c) is available online and is created by Plotly. 5 One can zoom in and rotate the 3D plot using the toolbar located at the upper right corner of the figure. The interactive version provides a better understanding of the direction of the bulk motion of the ejecta in 3D space.

Start interaction
Standard image High-resolution image Figure data file

We then calculated the average LOS velocity of the ejecta by averaging all the velocities obtained from different lines using both methods at each time step during the period of 15:26:30–15:34:30 UT. The average LOS velocity is 423 km s−1 with a standard deviation of 40 km s−1, which we take as the uncertainty of the LOS velocity.

3.4. Full Velocity of the Mass Ejection

We have obtained the POS velocity vPOS from the viewpoint of STEREO-A using time-distance diagrams in Section 3.1. We have also estimated the LOS velocity vLOS using SDO/EVE observations around the Earth in Section 3.3. The full velocity of the bulk motion of the ejecta was then computed by combining these two velocities.

As the POS velocity is measured in the HPC system, we first converted it to the HEE system. We projected the POS velocity in the ecliptic plane (i.e., the xy plane of the HEE system) and perpendicular to the ecliptic plane (i.e., the z-axis direction of the HEE system). The deviation of STEREO-A from the ecliptic plane, which is 0fdg075 at 15: 30 UT on 2021 October 28, can often be ignored as it is less than around 0fdg13 throughout the STEREO era. Hence the z-axis of the HPC system is in the ecliptic plane. Because the z-axis is perpendicular to the xy plane, the ecliptic plane containing the z-axis is perpendicular to the xy plane of the HPC system. Therefore, the projections of the POS velocity vPOS in and perpendicular to the ecliptic plane are still in the xy plane of the HPC system. The angle between the +x-axis direction of the HPC system and the ecliptic plane (denoted as α) and the angle between the POS velocity and +x-axis direction (i.e., θ in Equation (2)) can be directly added together to obtain the angle between the POS velocity and the ecliptic plane (denoted as θPOSP). From the angle between the +z-axis of the HEE system and +x-axis of the HPC system, α was derived to be around 1fdg6, indicating that the +x-axis of the HPC system is north to the ecliptic plane. Therefore, θPOSP turned out to be around −16fdg2, which is negative meaning that the POS velocity is south to the ecliptic plane. The projected speeds of vPOS in and perpendicular to the ecliptic plane can be calculated by,

Equation (6)

Equation (7)

where vPOSE, around 564 km s−1, is in the ecliptic plane and vPOSP, around 163 km s−1, is perpendicular to the ecliptic plane. It is also worth noting that the direction of vPOSE is perpendicular to the Sun-STEREO-A line (i.e., the z-axis of the HPC system).

We combined vLOS, vPOSE, and vPOSP to acquire the full velocity of the bulk motion of the ejecta. First, we calculated the projected speed of full velocity of the ejecta in the ecliptic plane. A sketch for the geometry used in the calculation is displayed in Figure 8(b). We denoted the projected speed in the ecliptic plane as vE and the angle between the propagation direction of the ejecta and the Sun–Earth line in the ecliptic plane as θE. The angle between the Sun-STEREO-A line and the Sun–Earth line measured in the ecliptic plane (θSTA) is around −37fdg5. So we have,

Equation (8)

from which we derived

Equation (9)

The projected speed in the ecliptic plane (vE) is then obtained by Equation (8). Second, we acquired the propagation direction and the full speed of the bulk motion of the ejecta by combing the velocities in and perpendicular to the ecliptic plane. The projected speed perpendicular to the ecliptic plane (denoted as vP) equals vPOSP; thus the full velocity of the bulk motion of the ejecta can be calculated as

Equation (10)

Equation (11)

where v is the full speed of the ejecta and θP is the angle between the true velocity vector and the ecliptic plane. Negative θP indicates that the full velocity is south to the ecliptic plane. The direction of the bulk motion of the ejecta is described by θE and θP. A 3D interactive version of the full velocity calculation is available with a snapshot shown in Figure 8(c). All the velocity vectors are moved to the origin of the HEE system for plotting but it is worth noting that the ejecta originates from the AR, which is located near the central meridian in the southern hemisphere of the Sun. The full velocity of the bulk motion of the ejecta was found to be around 596 km s−1 with a propagation direction of around 42fdg4 west to the Sun–Earth line in the ecliptic plane and 16fdg0 deviating to the south of the ecliptic plane.

The above derivation of the full velocity becomes unusable when ∣θSTA∣ equals 90°. Under this condition, the POS velocity will lie in the x-z plane of the HEE system and the solution of the full velocity is not unique. Also, the uncertainty in the full velocity estimation becomes fairly large when ∣θSTA∣ is close to 90°.

4. Summary

We have investigated signatures of a solar eruption on 2021 October 28, in the full-disk integrated spectra of He i 58.43 nm, O iii 52.57 nm, O v 62.96 nm, O vi 103.19 nm, Ne vii 46.52 nm, and Ne viii 77.03 nm observed by SDO/EVE. Intensities of all lines except O iii 52.57 nm experience hours-long dimmings after the flare, suggesting mass loss from the relatively lower solar atmosphere compared to normal CMEs. Obvious secondary components have been identified in the blue wings of O iii 52.57 nm, O v 62.96 nm, and Ne vii 46.52 nm during the impulsive phase and shortly after the flare's peak, which is in accordance with the appearance of the mass ejection. A double Gaussian fitting and RB asymmetry analysis suggest that the mass ejection has a LOS velocity of around 423 km s−1 from the Earth viewpoint. With EUV imaging observations in the 304 Å passband, we have also obtained the POS velocity of the ejecta from the STEREO-A perspective. Combing these two velocity components, the full velocity of the bulk motion of the ejecta has been found to be ∼596 km s−1 with an angle of 42fdg4 west to the Sun–Earth line in the ecliptic plane and 16fdg0 south to the ecliptic plane.

Our finding suggests that high-resolution spectroscopy at the EUV wavelengths has the potential to reveal the LOS velocities of CMEs. Combining the POS velocities inferred from EUV imaging observations, one could determine the true velocities of CMEs during their early propagation phases, which should significantly improve the accuracy of CME arrival time forecasting. The full-disk integrated spectra observed by EVE also provide a good opportunity to study the Sun as a remote star and improve our understanding of signals in the spectra from other stars. Our finding suggests that we may detect stellar CMEs through high-resolution spectroscopy, even though we cannot spatially resolve these features. This will be of great importance as stellar CMEs are the main drivers of exoplanetary space weather, which can significantly affect the habitability of exoplanets. Our future work will be focused on searching for the CME-related signals and estimating the physical parameters of CMEs through full-disk integrated spectra from both the Sun and other stars. We may also combine CME models and theoretical spectra synthesis to examine the feasibility of detecting the blueshifted secondary components in full-disk integrated spectra under different CME parameters and instrumental conditions.

This work is supported by the National Key R&D Program of China No. 2021YFA0718600, NSFC grants 11825301 & 11790304. We would like to acknowledge the data use from GOES, SDO, and STEREO/SECCHI. SDO is a mission of NASA's Living With a Star Program. Data from STEREO/SECCHI are produced by the consortium of RAL (UK), NRL (USA), LMSAL (USA), GSFC (USA), MPS (Germany), CSL (Belgium), IOTA (France), and IAS (France). We appreciate the helpful discussion with P. C. Chamberlin, Li Feng, and Beili Ying. We also thank the anonymous referee for their constructive comments and suggestions.

Footnotes

Please wait… references are loading.
10.3847/1538-4357/ac69d5