THE NATURE OF CME-FLARE-ASSOCIATED CORONAL DIMMING

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Published 2016 June 27 © 2016. The American Astronomical Society. All rights reserved.
, , Citation J. X. Cheng and J. Qiu 2016 ApJ 825 37 DOI 10.3847/0004-637X/825/1/37

0004-637X/825/1/37

ABSTRACT

Coronal mass ejections (CMEs) are often accompanied by coronal dimming that is evident in extreme ultraviolet (EUV) and soft X-ray observations. The locations of dimming are sometimes considered to map footpoints of the erupting flux rope. As the emitting material expands in the corona, the decreased plasma density leads to reduced emission observed in spectral and irradiance measurements. Therefore, signatures of dimming may reflect the properties of CMEs in the early phase of their eruption. In this study, we analyze the event of flare, CME, and coronal dimming on 2011 December 26. We use the data from the Atmospheric Imaging Assembly on the Solar Dynamics Observatory for disk observations of the dimming, and analyze images taken by EUVI, COR1, and COR2 on board the Solar Terrestrial Relations Observatory to obtain the height and velocity of the associated CMEs observed at the limb. We also measure the magnetic reconnection rate from flare observations. Dimming occurs in a few locations next to the flare ribbons, and it is observed in multiple EUV passbands. Rapid dimming starts after the onset of fast reconnection and CME acceleration, and its evolution tracks the CME height and flare reconnection. The spatial distribution of dimming exhibits cores of deep dimming with a rapid growth, and their light curves are approximately linearly scaled with the CME height profile. From the dimming analysis we infer the process of the CME expansion, and estimate properties of the CME.

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1. INTRODUCTION

Flares and coronal mass ejections (CMEs) are manifestations of the most energetic large-scale solar eruptions and often occur together. In addition, CMEs are the main source of strong geomagnetic storms. Geomagnetic storms can also be caused by corotating interaction regions (Balogh et al. 1999) when height speed solar streams emanating from coronal holes interact with streams of lower speed. During the eruptive events, transient coronal holes, or coronal dimmings, are often observed (Thompson et al. 2000; Harrison et al. 2003; Zhukov & Auchère 2004). Coronal dimming was first observed in Skylab data and characterized as transient coronal holes (Rust & Hildner 1976; Rust 1983). Subsequently, similar observations have been analyzed to study the relationship of dimming with CMEs, flares, and other associated phenomena (Hudson et al. 1996; Sterling & Hudson 1997; Harrison et al. 2003; Zhukov & Auchère 2004). By these series of studies, dimmings are usually interpreted as mass depletion due to the loss or rapid expansion of the overlying corona (Hudson et al. 1998; Harrison & Lyons 2000; Zhukov & Auchère 2004). This interpretation is supported by imaging observations of simultaneous and co-spatial dimming in several coronal lines (e.g., Zarro et al. 1999; Sterling et al. 2000), as well as spectroscopic observations (Harra & Sterling 2001; Tian et al. 2012). Although CMEs are also observed to occur without dimming, Reinard & Biesecker (2009) found that non-dimming CMEs all have speeds of less than 800 km s−1, suggesting a more intimate connection between fast CMEs and dimming properties. Krista & Reinard (2013) found further correlations between the magnitudes of dimmings and flares, and the CME mass by studying variations between recurring eruptions and dimmings.

Coronal dimming can be produced by various processes, although the main contributor is mass depletion. As summarized by Mason et al. (2014), several different mechanisms have been proposed to explain coronal dimming. (1) Mass-loss dimming: the mass-loss dimming is produced by the ejection of emitting plasma (Harrison & Lyons 2000; Harra & Sterling 2001), which causes darkening of the areas in and near the erupting active region. Harrison et al. (2003) showed that the coronal mass estimated from dimming signatures can account for a large percentage of the CME mass. Additional observations from the Hinode and Solar Dynamics Observatory (SDO) spacecraft have confirmed that the coronal plasma density decreases with accompanying outflows (Attril et al. 2010; Harra et al. 2011; Tian et al. 2012). (2) Thermal Dimming: this is due to the heating of coronal plasmas to higher temperatures, so that heated areas appear dark in extreme ultraviolet (EUV) or soft X-ray (SXR) channels sensitive to lower temperatures, but these areas are brightened simultaneously in channels sensitive to higher temperatures. (3) Obscuration Dimming: here the physical process that results in apparent dimming is an absorptive material (e.g., a filament) moving between bright materials (e.g., flare arcade) and the observer. (4) Wave Dimming: one of the simplest explanations of the observations is that plasma is compressed as a longitudinal wave passes through the medium. (5) Doppler Dimming: if the plasma is moving with a line of sight motion component, the coronal emission lines are Doppler-shifted, which may cause reduction of the total counts observed in a filtergram with a fixed and narrow bandpass, leading to an apparent dimming in the data.

Among these mechanisms the mass-loss dimming is considered to be the main process of coronal dimming, and this scenario is supported by many recent studies (Sterling & Hudson 1997; Reinard & Biesecker 2008, 2009; Aschwanden et al. 2009). Post-flare dimmings detected by the EVE instrument on SDO are used to estimate the CME mass (Hudson et al. 2014). Based upon earlier X-ray observations, Hudson et al. (2014) interpret these dimmings as the result of a CME mass ejection from the low corona. They estimate the mass from the dimming by deriving a best pre-event temperature and emission measure in the dimmed region from EVE, and a source volume from Atmospheric Imaging Assembly (AIA) images. Tian et al. (2012) suggest that dimming is mainly an effect of density decrease rather than temperature change by plasma diagnostics of the dimming region. The mass losses in dimming regions have been estimated from two different methods, and they makeup 20%–60% of the masses of the associated CMEs, suggesting that a significant part of the CME mass indeed comes from the region where the subsequent dimming occurs. The mass flux carried by the outflows has also been estimated from observations.

Considering that dimmings map the footpoints of erupting flux ropes, the magnetic flux in dimming regions is measured to estimate the total flux in the flux rope (Webb et al. 2005; Qiu et al. 2007). Detailed analysis of dimming observations also demonstrate an evolution of dimming in terms of both the area of dimming regions and the depth of dimming. Miklenic et al. (2011) reported a twin-dimming event near the feet of an erupting sigmoid CME, both of which also expanded in area. They interpret such evolution as due to the interaction of erupting flux rope with overlying field lines. Downs et al. (2015) conducted comprehensive, data-driven numerical simulations and topological analysis of coronal dimmings associated with an erupting flux rope, and demonstrated three types of coronal dimming and their evolution. The first two types of dimming map the feet of the erupting rope, or of overlying field lines reconnecting with the rope and subsequently entrained into the erupting rope. The third type of dimming maps the feet of the arcade adjacent to the rope, which does not erupt. These studies suggest that coronal dimming evolution is related to the reconstruction of magnetic structures during the flux rope eruption. Therefore, analysis of dimming observations can provide some measurements of CME properties.

It is widely accepted that energy stored in the magnetic field is released to the solar atmosphere by magnetic reconnection. Subramanian & Vourlidas (2007) showed that, on average, the magnetic energy contained in CMEs provides at least 74% of what is required for their propagation from the Sun to the Earth. A large majority of CMEs observed with coronagraphs are now confirmed to possess a flux rope morphology (e.g., Vourlidas et al. 2013; Zhang et al. 2013). Many studies are focused on figuring out the CME evolution from a 3D viewpoint (Thernisien et al. 2009; Gopalswamy et al. 2012; Subramanian et al. 2014). They study the CME evolution based on different models and for varied purposes. Although there has been some observational evidence for the fact that some flux rope CMEs expand in a self-similar manner in the coronagraph field of view (Poomvises et al. 2010; Kilpua et al. 2012; Colaninno et al. 2013), there are still some events which cannot be described in a self-similar expansion model. Self-similarity has been invoked in a number of theories of CME propagation (e.g., Kumar & Rust 1996; Démoulin & Dasso 2009; Wang et al. 2009; Olmedo & Zhang 2010). Other models, such as the full ice-cream cone, partial ice-cream cone, and flat cone models, are used to describe propagations of some CMEs (Gopalswamy et al. 2012).

In this paper, we analyze observations of a coronal dimming event associated with a halo CME and a two-ribbon flare on 2011 December 26. Observations are obtained by the SDO and the Solar Terrestrial Relations Observatory (STEREO). We find two dimming regions at opposite ends of two flare ribbons, which probably map the feet of the erupting CME, and also a dimming band along a flare ribbon, which may map the feet of the magnetic arcade overlying the erupting CME. Our analysis shows that the time profiles of coronal dimming at various locations well track the CME height evolution and magnetic reconnection. The spatial distribution of dimming exhibits cores of deep dimming, whose evolution appears to agree with the prediction by a one-dimensional isothermal CME expansion model in the early phase of the eruption. The paper is organized as follows. Observations are described in Section 2, followed by data analysis and results in Section 3. Discussions and conclusions are given in Section 4.

2. OBSERVATIONS

In this study, we analyze an eruptive event on 2011 December 26. A C-5.7 flare takes place in AR 11384 at N17 W02. It is associated with a fast halo CME as well as coronal dimming. In the event, the flare and coronal dimming take place near the disk center, and are observed by the SDO's (Pesnell et al. 2012) AIA (Lemen et al. 2012; see Figure 1). AIA is a full-disk imager observing in seven EUV and two UV bandpasses with a moderate cadence (12 s in EUV channels and 24 s in UV channels) and high resolution (0farcs6 pixel−1 spatial scale). The Helioseismic and Magnetic Imager (HMI; Schou et al. 2012) on board SDO measures magnetic fields in the Sun's photosphere. HMI observes the full solar disk at 6173 Å with a spatial scale of 0farcs5 pixel−1. The magnetic reconnection flux is measured during the flare by summing up the magnetic flux encompassed by flare ribbons (Qiu et al. 2002, 2004).

Figure 1.

Figure 1. AIA images taken at peak times of given passbands for the 2011 December 26 event. The two-ribbon flare is located at the solar disk center and ribbon brightening spreads along the polarity inversion line from southwest to northeast. Post-flare loops are clearly seen in multiple EUV channels.

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The CME that is associated with the flare is observed by STEREO. STEREO is a pair of counter-rotating Sun satellites at roughly 1 astronomical unit (au) from the Sun. The Extreme UltraViolet Imager (EUVI; Wuelser et al. 2004) observes the full solar disk in 304, 171, 195, 284 Å, in field of view to 1.7 ${R}_{\odot }$ with a spatial scale of 1farcs6 pixel−1. The inner (COR1) and outer (COR2) (SECCHI; Howard et al. 2008) white light coronagraphs provide images from 1.5 to $4\;{R}_{\odot }$ and out to $15\;{R}_{\odot }$, respectively. In 2011, the STEREO A and B are located at positions about ±90° from the SDO, providing a very good opportunity to simultaneously observe flares, coronal dimmings, and magnetic fields on the Sun's disk, and CME propagation from the limb. In this study we use observations by EUVI, COR1, and COR2 on STEREO to track the height of the CME (Figure 2), and examine its evolution together with the flare and coronal dimming.

Figure 2.

Figure 2. CME evolution observed by STEREO EUVI, COR1, and COR2. A very bright core is clearly seen from COR1.

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3. DATA ANALYSIS & RESULTS

3.1. Flare, CME, and Magnetic Reconnection

The eruptive event takes place near the disk center. It produces a C-5.7 flare. According to the GOES catalog,4 the soft X-ray (1–8 Å) emission of the flare starts to rise at 11:23 UT, peaks at 11:50 UT, and lasts until 12:18 UT. The flare is well observed by SDO/AIA. Figure 1 gives an overview of the flare in nine UV/EUV wavelengths. Each image is taken at the peak time of the total emission in the given bandpass. The flare is a very typical two-ribbon flare, with brightening of the two ribbons visible in multiple passbands. The ribbon brightening quickly spreads from southwest to northeast along the magnetic polarity inversion line (PIL), and then expands outward away from the PIL. Such a time sequence of ribbon brightening is displayed in Figure 3, superimposed on a longitudinal magnetogram obtained by SDO/HMI before the flare onset. Subsequently, post-flare loops are clearly seen in the EUV channels. The light curves observed by AIA for the flaring region are displayed in the top panel in Figure 4. The figure shows that UV and EUV emissions at the flare ribbons, particularly in the 1600 and 304 Å bands, start to rise at around 11:10 UT, 10 minutes before the rise of the GOES SXR emission. In the plots, the vertical dashed lines indicate the start of the flare ribbon brightening, as well as the start and peak times of the soft X-ray emission observed in GOES, respectively.

Figure 3.

Figure 3. Longitudinal magnetogram of the flaring region from SDO/HMI. The colors indicate the time sequence of flare ribbon brightening after 11:00 UT, and the three boxes indicate regions of interest where dimming is primarily located. Dimming pixels are selected from these regions for further analysis in the following figures.

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Figure 4.

Figure 4. Upper: integrated EUV counts over the flaring region shown in Figure 1, and the GOESSXR light curve. All light curves are normalized to the maximum. Three vertical lines indicate the times for the start of the flare ribbon brightening, and the rise and peak of the GOESSXR emission. Middle: CME height, derived velocity, magnetic reconnection flux, and total EUV counts in 193 and 171 bands of dimming pixels in the active region. Bottom: derived CME acceleration and magnetic reconnection rate.

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According to the standard flare model (Carmichael 1964; Sturrock 1966; Hirayama 1974; Kopp & Pneuman 1976), the expansion of flare ribbons indicates a progressive reconnection that continuously forms flare loops. From the flare ribbon evolution, we can measure the reconnection rate by summing up the magnetic flux in newly brightened UV pixels (Fletcher & Hudson 2001; Qiu et al. 2002, 2004; Saba et al. 2006; Qiu et al. 2010). An automated procedure has been developed to identify flaring pixels and minimize measurement uncertainties caused by fluctuations in photometry calibration and by non-flaring signatures (Qiu et al. 2010). We use the SDO/HMI LOS magnetogram combined with the SDO/AIA 1600 Å images of flare ribbon evolution (see Figure 3) to derive the magnetic reconnection flux and magnetic reconnection rate, which are displayed in the middle and bottom panels of Figure 4, respectively. The calculation is made between 11:00:00 UT and 13:20:00 UT. In this flare the uncertainty in reconnection flux measurement is about 40%, mostly caused by the imbalance between the measured positive and negative fluxes, although the two fluxes well track each other during the flare evolution. At 11:10 UT when ribbon brightening starts, the reconnection flux starts to rise, and the total reconnection flux is measured to be 1.8 × 1021 Mx. The reconnection rate is the time derivative of the reconnection flux, which amounts to 1.5 × 1018 Mx s−1 at around 11:30 UT.

The associated CME is a partial halo CME observed by LASCO with an average speed of 736 km s−1 in the LASCO C2 and C3 field of view, according to the LASCO CME catalog by the Coordinated Data Analysis Workshops (CDAW)5 CME catalog (Gopalswamy et al. 2009). The CME event, particularly in its early stage, is best observed by the STEREO instruments from the limb. Figure 2 shows the CME evolution observed by EUVI, COR1, and COR2 on board STEREO. The CME is first seen at 11:06:25 UT as a faint loop structure in the running difference images at 195 Å by EUVI-B, and expands afterwards. The bright CME front is clearly seen in COR1 at 11:30:55 UT. Five minutes later, a bright core beneath the front also appears in the COR1 field of view. These structures can also be identified in COR2 images from 12:24:55 UT.

To measure the height of the CME, we track the position of the leading edge of the CME along a guide line, indicated in the figure, in the direction of its ejection. The CME leading edge is best visible in the running difference images by EUVI, COR1, and COR2. This position is tracked manually several times. The mean and standard deviation of these measurements are presented in the figure as the CME height and its uncertainty, respectively. The middle panel of Figure 4 shows the measured height (starting from the solar center) of the CME front together with the reconnection flux measured from the flare ribbon evolution. We derive the CME velocity using a linear fit to every four consecutive points, in order to reduce large fluctuations in the original measurements. The uncertainty indicated in the velocity plot is the standard deviation of this linear fit. The plot shows that the CME starts moving slowly at a speed below 100 km s−1 when the flare UV emission starts, and then speeds up in the next 10 minutes. It achieves the maximum velocity of about 1000 km s−1 around the time of the GOES soft X-ray emission peak, when the increase of the reconnection flux starts to slow down substantially. The CME then moves at a relatively constant speed of about 700 km s−1 for the next few hours. The CME velocity profile shows a temporal correlation with the reconnection flux as well as the GOES soft X-ray light curve during the rise phase, consistent with previous observations of the timing relationship between fast CMEs and flares (Zhang et al. 2001; Qiu et al. 2004; Patsourakos et al. 2010, 2013; Cheng et al. 2014). The CME acceleration is also estimated and compared with the magnetic reconnection rate. The bottom panel of Figure 4 shows that these two quantities exhibit similar evolution trends. The CME acceleration peaks around 11:30 UT with a peak value of 0.4 km s−2, and diminishes after 12:00 UT, when flare reconnection has also stopped. At these times when acceleration/reconnection starts (11:10 UT), peaks (11:30 UT), and stops (12:00 UT), the front of the CME is at 0.2, 1, and 3 solar radii above the surface, respectively.

In summary, these observations show the following stages of the CME and flare evolution:

  • 11:10 start of flare ribbon emission, CME motion, and reconnection;
  • 11:20 start of SXR rise, significant CME acceleration, and fast reconnection;
  • 11:30 peak of CME acceleration and reconnection rate;
  • 12:00 peak of SXR emission and CME velocity, and reconnection diminished.

In the standard flare-CME model, energy stored in the magnetic field is released by magnetic reconnection to heat flare plasmas, as well as to accelerate the CME. The observed coincidence between the CME evolution and magnetic reconnection, within the uncertainty of a few minutes, suggests that acceleration of the CME is related to the reconnection process.

3.2. EUV Dimming

3.2.1. Temporal and Spatial Evolution

Coronal dimming is often observed to accompany CMEs. In this event, dimming signatures are observed in AIA images of several EUV bands, most prominently 171, 193, 211, and 335 bands, suggesting that the characteristic temperature of the dimming areas ranges between 1 and 3 MK. By checking the full disk images, the most significant dimming occurs near the flare region. No other obvious dimming is detected during that time.

In the middle panel of Figure 4, we plot the 171 and 193 light curves produced from pixels exhibiting dimming. The pre-dimming counts level in these pixels is within ${I}_{q}\pm \sigma $, Iq and σ being the median counts and standard deviation, respectively, of a control region free of coronal loops, and EUV counts in these pixels keep decreasing continuously for a few minutes. In this way, we exclude apparent dimming signatures due to removal or motion of overlying coronal loops during the eruption (Qiu et al. 2007; Hock et al. 2010, 2012; Harra et al. 2011). The plots show that coronal dimming evolves along with the flare reconnection and CME eruption. EUV emission in the 193 passband starts to decrease quickly at 11:15 UT, 5 minutes after the start of the flare reconnection and CME takeoff, whereas dimming in the 171 band starts about 5 minutes later. The maximum dimming occurs around the peak time of the GOES SXR emission as well as the CME velocity, and then the EUV emission in these dimming regions starts to rise as post-flare loops form in these regions.

To study the evolution of dimming and its relation to the eruptive flare, Figure 5 gives an overview of the flare region in three different passbands by AIA in 171, 131, and 304 Å at several critical times during the flare/CME evolution. The dimming pixels selected above mostly locate in EUV moss areas adjacent to the flare ribbons. One dimming region is found at the left end of the flare ribbon in the positive magnetic fields. Dimming also occurs at the right end of the conjugate flare ribbon in the negative magnetic fields. These two regions are indicated by the rectangular boxes in Figure 5, as well as in the magnetogram in Figure 3. We also find a band of dimming region along the flare ribbon in the positive magnetic fields, indicated by the long parallelogram in Figure 3. These regions are denoted as "LF" (left foot), "RF" (right foot), and "RB" (ribbon) in the figures as well as the following text. Dimming is also visible along the other ribbon in the negative magnetic fields, but not as outstanding and widespread as in the RB region, perhaps because of projection effects given the disk position of the active region. Seen in the leftmost panels of Figure 5, before the flare, these regions are characterized by EUV moss structures at the base of the corona, and are mostly free from overlying coronal loops. After the eruption, the moss structure in some areas is removed, causing coronal dimming seen in a few EUV bands including the 304 Å band observing the transition region, as shown in the rightmost panels of the figure.

Figure 5.

Figure 5. Snapshots of flare and dimming evolution in three different passbands (171, 131, and 304 Å ) at six times. The boxes indicate regions of interest where we study dimming signature in details. The four slices sample different dimming regions, and stack plots in the next figure are constructed along these slices to study the tempo-spatial variation of dimming.

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To analyze the temporal and spatial pattern of dimming evolution we sample pixels in these regions by generating stack plots of EUV emissions in a few passbands along a few slices across these regions. These slices are marked in Figure 5. The left and middle panels in Figure 6 show the stack plots of EUV counts along slices AB and CD, which are placed along and across the dimming band RB next to the flare ribbon, respectively. The right panel shows the stack plots along slices EF and GH, which sample the two dimming regions at the ends of the conjugate ribbons. From top to bottom, the plots are generated for the AIA 131, 335, 193, 171, and 304 Å passbands, sampling plasma emission at different temperatures. Each stack plot is normalized to the EUV counts at 10:00:12 UT. The two vertical dashed lines indicate the times at 11:10 UT and 11:30 UT, respectively, when CME acceleration and flare reconnection start and peak.

Figure 6.

Figure 6. Dimming evolution along the marked slices in Figure 5. Two vertical lines indicate times at 11:10 and 11:30 UT, respectively. Dimming occurs in multiple EUV bands, and major dimming starts after 11:10 UT.

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Seen in these plots, dimming is observed in multiple EUV bands including the EUV 304 Å band. In most dimming pixels, significant dimming starts after the flare/CME onset (11:10 UT) in the 335 and 304 passbands, and even later in other wavelengths. In a few locations, gradual dimming appears to occur before 10:30 UT. The middle panel of Figure 6 sampling the evolution across the flare ribbon along slice CD also shows apparent spreading of dimming away from the PIL, followed by spreading of ribbon brightening. For example, seen in the 193 Å passband, between 11:25 and 11:35 UT, the dimming front along the ribbon spreads away from the PIL at the speed of about 10 km s−1. On the other hand, the right panel shows that dimming along the EF and GH slices across the LF and RF regions also spreads out, but these pixels are not brightened later on.

The temporal and spatial evolution of dimming in multiple wavelengths suggests that dimming in these regions is not caused by thermal dimming or disruption of pre-flare active region loops (Hock et al. 2010; Harra et al. 2011), neither do they appear to be obscured by absorptive materials. Most likely, dimming is caused by density decrease due to expansion of corona structures anchored at these locations. Specifically, the LF and RF regions at the two ends of the flare ribbons locate at oppositely curved magnetic elbows that loop out on opposite ends of the neutral line (Sterling & Hudson 1997; Moore et al. 2001), and likely map the footpoints of the erupting CME, similar to the event reported by Webb et al. (2000). On the other hand, the narrow band of dimming along the outer edges of flare ribbons is brightened afterwards. The morphology evolution at these locations much resembles the scenario depicted by Forbes & Lin (2000), Švestka (1996), and Moore et al. (2001), where the erupting flux rope stretches the overlying coronal arcade, causing dimming at the feet of the arcade; the stretched field lines then reconnect and form closed loops, and therefore these locations are brightened due to heating along closed loops. Note that at these locations, reconnection as inferred from the ribbon brightening starts after the dimming; yet in other regions, such as in the inner part of the flare ribbons, reconnection takes place much earlier, and dimming is not observed in some of these regions. As a result, the global signature of significant dimming appears to occur after the onset of reconnection.

3.2.2. Coronal Dimming versus CME Evolution

To further examine the timing of coronal dimming with respect to the CME eruption, we analyze the EUV light curves of the three regions, with a focus on the 193, 171, and 304 passbands that observe the base of the corona. The AIA response functions for the 193 and 171 bandpasses each have a dominant single peak at temperatures below 10 MK (Boerner et al. 2012), so observations in these passbands provide a more reliable estimate of the characteristic temperature of the dimming plasma. Light curves of the 211 passband are very similar to those at the 193 passband and are therefore not presented. Emission in the 304 Å passband includes a large contribution of the He ii 304 Å line that forms in the transition region or upper chromosphere at a characteristic temperature of about 0.1 MK. Traditionally, dimming is not often studied in this wavelength, but we present observations in this wavelength as a reference. Observations show that dimming is also visible in the 304 band, likely caused by the diminished transition-region emission due to decreased coronal pressure along expanding field lines anchored at these locations.

In the top row of Figure 7, we plot light curves of the total EUV counts from all pixels in the LF (left), RF (middle), and RB (right) regions, respectively. Each light curve is normalized to the pre-eruption counts at 10:00 UT. In the second row, the inverse of the same light curves are presented, in order to compare with the CME height profile overplotted in symbols. In these light curves, the 171 total counts appear to be rising (brightening) rather than decreasing (dimming), partly because not all pixels in the regions are dimming. We select pixels that show evidently and continuously decreased counts, or dimming, in each bandpass during the eruption, and compare their light curves with the CME height profile. We also find that, in the 171 passband, a significant number of selected dimming pixels in all three regions exhibit a brief brightening before dimming. This will be discussed later. Light curves from two groups of dimming pixels are presented in the following four rows of the figure.

Figure 7.

Figure 7. EUV light curves for the LF (left), RF (middle), and RB (right) regions indicated in Figure 3. From top to bottom: the first two rows show light curves for all the pixels and its inverse light curves, the middle two rows show light curves and their inverse for the pixels that show continuous dimming, and the bottom two rows show light curves in dimming pixels that also exhibit brightening in 171 band before dimming. Symbols with error bars show the CME height measured from STEREO observations.

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In the third and fourth rows we show light curves of the total counts of the first group of pixels that exhibit dimming in both the 193 and 171 bandpasses without brightening before dimming. In the bottom two rows we plot light curves of the second group of pixels with dimming in both bandpasses but also significant brightening in the 171 passband before dimming. All these light curves show a rapid decrease of EUV counts in the 193 and 171 bands at or after the onset of fast CME acceleration at around 11:10 UT. Dimming well tracks the CME height for about 20 minutes, and the slope of the dimming growth, namely the rate of the counts decrease, particularly in the 193 bandpass, is comparable with the growth rate of the CME height. When the two groups of the dimming light curves are compared it appears that the dimming slope of the 193 light curve in the second group, which show significant brightening in the 171 band before dimming, is slightly larger than in the first group. Finally, in some regions and at some wavelengths, gradual dimming starts earlier, well before 11:00 UT, consistent with the stack plots in Figure 6.

If coronal dimming results from the decreased density in expanding coronal structures, the dimming light curve at a given location is related to the height of the structure anchored at that location. It is not possible to identify expanding coronal structures anchored at different locations or pixels of dimming; however, we may use the measured CME height as a common reference to examine the growth of dimming in various places. For this purpose we make a routine to select and fit the dimming light curve in each of the three bandpasses (193, 171, and 304) in each dimming pixel as related to the CME height by the following function

Equation (1)

where I refers to the EUV counts in a given pixel observed by AIA, and H is the CME height above the solar surface measured in STEREO observations. I0 and H0 are values at 11:06 UT when the CME is first visible in STEREO observations. The fitting parameter, α, gives the slope, or the growth rate, of dimming relative to the growth of the CME height, both of which are interpolated to a grid of 1 minute time cadence. For each pixel, fitting is performed in the time range when EUV counts monotonically decreases (i.e., dimming). The period of pre-dimming brightening is excluded from fitting, and obviously the gradual dimming period before the CME is visible is also excluded. In some pixels, post-eruption dimming apparently evolves in two stages, with a rapid first-stage dimming followed by a gradual dimming. In this case, fitting is performed in two stages, and we use α from the first stage.

Figure 8 shows the statistics of the fitting parameter, α, for a few thousand dimming pixels in the three regions. The fitted slope mostly ranges between 0.4 and 1.2, although different regions show small variations. Goodness of fit is measured by ${\chi }^{2}$, and we accept fitting results with ${\chi }^{2}\leqslant 2$. The uncertainty in the fitting parameter, α, is about 0.2. For the LF region (left panel), about 75% of pixels show dimming in 193 Å, 25% of pixels show dimming in 171 Å, and 20% of pixels show dimming in 304 Å, the median of the dimming slope (α) being 0.45, 0.36, and 0.39, respectively. For the RF region (middle panel), about 85%, 36%, and 39% of pixels show dimming in 193 Å, 171 Å, and 304 Å, the median of the slope being 0.5, 0.4, and 0.3 for the three passbands. For the RB region along the flare ribbon (right panel), 73%, 39%, 36% of pixels show dimming in 193, 171, and 304 Å, and the median slope is 0.7, 0.5, and 0.3 for the three bands. Pixels with a larger slope usually exhibit stronger maximum dimming (i.e., lower counts). We also find that the dimming slope in the second group of pixels, which exhibit pre-dimming brightening, is statistically larger than in the first group.

Figure 8.

Figure 8. Histograms of the dimming slope, α, (see the text) from fitting dimming light curves in three regions, LF (left), RF (middle), and RB (right). The procedure of fitting is given in the text.

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We further study the spatial distribution of the fitted dimming slope by mapping α in Figure 9. Different colors indicate different α values, which are indicated in the figure. The fitted results for the three wavelengths (193, 171, and 304 Å) are displayed in the figure. We find more dimming pixels in 193 Å than in the other two wavelengths. A large percentage of pixels have a dimming slope between 0.4 and 1.2. A very small number of pixels have $\alpha \geqslant 1.6$. Generally, the slope in most pixels is less than 1.2, both in footpoint regions and along the flare ribbon. Interestingly, the map shows a certain pattern of the slope distribution, which is most evident in the 193 band. The right and left footpoint regions each exhibit a core of a large slope (i.e., deep dimming) shown in cyan and green colors, surrounded by outer layers in yellow and then red, indicating the dimming slope successively decreasing outward. The RB area also shows a regular pattern: from right to left as approaching the left foot along the ribbon, the slope becomes larger, from red (α = 0–0.4) to green (α = 0.8–1.2). Such a spatial pattern is also seen in the other two bandpasses, but it is not as prominent as in the 193 band.

Figure 9.

Figure 9. Spatial distribution of dimming slope α in three passbands. It exhibits a regular pattern with deep dimming cores at the ends of the two ribbons.

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In summary, we find that the dimming slope mostly ranges between 0.4 and 1.2, and its spatial distribution exhibits deep dimming cores, most evident in the 193 band, around the regions which probably map the CME feet. These results will be discussed in the following section in the context of the CME expansion process.

3.3. Coronal Dimming and CME Expansion

The fact that dimming curves well track the CME time height profile may indicate that dimming is related to the expansion of the CME. As the coronal structure expands, density decreases, so the emission measure along the line of sight decreases to produce diminished EUV emission. In the following, we test a few CME expansion models to investigate whether these models can explain the observed dimming signatures.

The AIA observed EUV emission in terms of data counts in a given pixel can be approximated by

Equation (2)

where L is the length along the line of sight, n and T are the mean electron density and temperature along L, and R(T) is the temperature response function of the AIA filter.

If the CME expansion is one-dimensional, for mass conservation, the plasma density inside the expanding coronal structure decreases linearly with the increasing L, namely $n\propto {L}^{-1}$. If we assume $L\sim H$, H being the CME height, for an isothermal model where plasma temperature, T, is constant, the observed EUV counts variation is related to the CME height by

Equation (3)

where n0, H0, and I0 are the initial values at 11:06 UT, when CME is first visible in the STEREO field of view. The CME height, H, is measured above the solar surface.

If the expansion is self-similar, the plasma density decreases with the increasing L by the relation $n\propto {L}^{-3}$. Again, assuming that $L\sim H$, in an isothermal model, we arrive at

Equation (4)

If on the other hand, the CME structure undergoes adiabatic expansion, then ${{TV}}^{\gamma -1}=\mathrm{const}.$, V being the plasma volume, with $\gamma =\tfrac{5}{3}$. For the one-dimensional expansion $V\propto L\propto {n}^{-1}$. Therefore,

Equation (5)

where L0 and T0 are the initial values at 11:06 UT. With $L\sim H$, the observed EUV counts change as

Equation (6)

For an adiabatic self-similar expansion, we have

Equation (7)

and

Equation (8)

With these models, we estimate the observed dimming evolution ($I/{I}_{0}$) as related to the measured height $H/{H}_{0}$ of the CME. First, applying the filter ratio method to AIA data at 171, 193, and 211 Å, we find the plasma temperature ${T}_{0}=1.4$ MK at 11:06 UT, which is a reasonable active region coronal temperature. In the isothermal model, $T={T}_{0}=1.4$ MK. In the adiabatic model, T varies as described by Equations (5) and (7) for the one-dimensional and self-similar expansion, respectively. As the CME propagates, the derived temperature decreases to ${10}^{5.5}$ K or even lower. Then, from Equations (3), (4), (6) and (8), we calculate the EUV light curves $I/{I}_{0}$ as would be observed in the AIA 171 and 193 passbands for the four different CME expansion models. From the analysis above, if the CME expansion is isothermal, the EUV counts monotonically decrease as the CME expands by ${I}_{0}/I\sim {(H/{H}_{0})}^{\alpha }$, and the power index, α, should be one for the one-dimensional expansion or five for the self-similar expansion in both the 193 and 171 bands. On the other hand, if the CME undergoes an adiabatic expansion as density decreases, the plasma temperature also decreases, so the EUV counts variation becomes a bit complicated. The response function for the 193 band peaks at around 1.5 MK, comparable with T0, so the adiabatic expansion will reduce the observed 193 counts further, more than in the case of isothermal expansion. Therefore, the predicted slope of the 193 dimming is greater than one in the one-dimensional expansion model and greater than five in the self-similar expansion model. In the 171 passband, the filter response function peaks at 0.8 MK, lower than ${T}_{0}=1.4$ MK, hence the predicted light curve for adiabatic expansion models is more complicated.

Figure 10 shows these modeled light curves in the 193 (left) and 171 (right) bands using Equations (3), (4), (6), and (8), in comparison with some observed light curves in the left footpoint region (top), right footpoint region (middle), and ribbon region (bottom). As discussed above, in the 193 band, the predicted light curves with adiabatic expansion models (blue and red) have a larger slope than isothermal expansion models (cyan and green), and in the 173 band, adiabatic expansion produces apparent brightening in the observed light curves, followed by a sharp dimming with a large dimming slope. As shown in the last section, the observed EUV light curves have the dimming slope, α, mostly ranging between 0.4 and 1.2, whereas the predicted EUV light curves should have slopes greater than one. Therefore, dimming in many pixels do not agree with any of the expansion models. In the figure we chose to plot the light curves of the pixels in dimming cores, which have relatively large slopes. For the three selected regions (LF, RF, RB), the 193 counts variation of these pixels most closely follows the 1D isothermal expansion model. In the 171 band, most of these same pixels appear to be brightened first, similar to the 1D adiabatic curve, and then the subsequent dimming curve again mostly resembles the 1D isothermal expansion model.

Figure 10.

Figure 10. Left: predicted dimming light curves in 193 (left) and 171 (right) bands based on different CME expansion models (colored lines), compared with observed dimming light curves from the dimming cores in the LF (top), RF (middle), and RB (bottom) regions.

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From the fitting result we can exclude the self-similar expansion process for this event, if expansion of the coronal structures anchored at the dimming locations can be approximated by, or linearly scaled with, the measured CME height. The core regions of deep dimming exhibit EUV light curves mostly tracking the 1D isothermal expansion model based on the measured CME height. It is not clear whether the observed initial brightening in the 171 band is caused by adiabatic expansion for the initial period, since light curves in the 193 band of the same pixels during that period do not follow the prediction by the adiabatic expansion model.

We can also estimate the mass and kinetic energy of the erupting CME, assuming that dimming is primarily caused by expansion of CME field lines anchored at these dimming locations. From the filter-ratio analysis mentioned above, we get the pre-eruption mean plasma temperature around 1.4 MK. The pre-eruption mean plasma density is estimated by

Equation (9)

and the total mass of the CME is

Equation (10)

where ${\rm{\Delta }}S$ is the area of a dimming pixel, and f1 is a scaling factor larger than one, since the half length of the structure is usually a few times the length scale along the line of sight L0. We may further write ${L}_{0}\approx {f}_{2}{H}_{0}$, with ${f}_{2}\lt 1$, indicating that L0 is a fraction of the CME height, H0. Combining the above equations, the CME mass is given as

Equation (11)

The values of f1 and f2 greatly depend on the geometry, including the aspect ratio of the CME structure. Since the CME structure before its eruption is hardly visible in the corona, its unknown geometry presents the largest uncertainty in the mass estimate. If the pre-eruption CME structure is approximated by a semi-circular loop with the axis of the loop in a plane perpendicular to the solar surface, and the major radius of the loop, which is the same as H0 in this geometry, is four times the minor radius of the loop, then ${f}_{2}\approx 0.5$, and ${f}_{1}\approx \pi $. With this geometry, the mean density is estimated to be ∼1.0 $\quad \times \quad {10}^{9}$ cm−3. By summing up all the dimming pixels, the total mass loss is $m\approx 1.1\quad \times $ 1015 g. The derived maximum CME velocity is about 1100 km s−1, yielding the maximum kinetic energy 6.9 × 1030 erg. If we consider that dimming along the other ribbon in the negative field is obscured by projection effects, the mass and kinetic energy could be increased, but by no more than a factor of two. In comparison, the CME mass and kinetic energy are estimated to be $4.3\times {10}^{15}$ g and $1.5\times {10}^{31}$ erg (using the mean speed of 736 km s−1), respectively, with the LASCO white light coronagraph observations (CDAW). An estimate from the dimming analysis appears to set a lower-limit of the CME mass, which is about one-quarter of the estimate from coronagraph observations. Such an estimate is very rough, subject to the uncertainties in f1 and f2 because of the unknown CME geometry; it is therefore only appropriate as an order-of-magnitude estimate.

Finally, we measure the magnetic flux encompassed by the dimming regions. In the entire active region, about 4% pixels exhibit dimming in both the 193 and 171 bands with the longitudinal magnetic flux density greater than ±10 G. The sum of the magnetic flux in these pixels amounts to $3.4\times {10}^{20}$ Mx in positive fields and $1.4\times {10}^{20}$ Mx in negative fields. Magnetic field in dimming pixels in the LF and RB regions is predominantly positive, and the field in the RF region is negative. That the negative flux is smaller than the positive flux is due to lacking dimming signatures along the flare ribbon in negative fields, most likely because of a projection effect. The total flux at the feet of the expanding field lines should be closer to the measured positive flux, which is about 20% of the total reconnection flux measured from flare ribbons.

4. DISCUSSIONS AND CONCLUSIONS

The analysis presented in this paper is focused on EUV dimming associated with an eruptive flare. Coronal dimming is observed near flare ribbons in multiple EUV passbands of AIA, together with a fast CME observed by STEREO. Significant dimming starts at or after the onset of the CME eruption or flare reconnection, and the dimming depth (decrease of EUV counts) grows as the CME propagates outward. The time sequence of the flare/CME/dimming event in the early phase of eruption is as follows: (1) 11:06 the CME is first seen by EUVI/STEREO; (2) 11:10 the start of the CME motion and reconnection; (3) 11:20 the start of significant CME acceleration, fast reconnection, and rapid dimming; (4) 11:30 the peak of the CME acceleration, reconnection rate, and strong EUV dimming; (5) 12:00 the peak of the CME velocity, GOES emission, and EUV dimming, whereas reconnection is diminished. Such timing among these events indicates that fast reconnection, CME expansion, and coronal dimming are intimately related.

The spatial distributions of the dimming signatures are also studied. Dimming is primarily located near flare ribbons. Two dimming regions are found at the opposite ends of the two ribbons, which likely map the conjugate feet of the CME. During the flare eruption, dimming along the outmost edges of one flare ribbon is also observed, which spreads outward at an apparent speed of ∼10 km s−1. It is followed by brightenings of flare ribbons. This signature agrees with the standard model that the overlying coronal arcade is stretched by the erupting CME, causing coronal dimming at the feet; the arcade then reconnect and produce brightening ribbons. Furthermore, we find that dimming regions exhibit deep dimming cores, where dimming grows more rapidly, and the dimming growth becomes smaller outside the cores. These signatures are similar to the MHD simulation results by Downs et al. (2015).

Our analysis of the EUV dimming in multiple wavelengths suggests that dimming in this event is most likely caused by plasma density depletion when overlying coronal structures expand. Assuming that the expansion of these structures anchored at the dimming locations can be approximated by the CME height measured from STEREO observations, we predict dimming light curves using four simple models, i.e., one-dimensional adiabatic, self-similar adiabatic, one-dimensional isothermal, and self-similar isothermal expansion models. Observed light curves in thousands of dimming pixels are compared with the model predicted light curves in the AIA 193 and 171 bands. We find that the dimming variation in the deep dimming cores well follows the predicted light curve by the 1D isothermal expansion model, in which case, the dimming variation is linearly scaled with the CME height. Dimming light curves outside the cores do not agree with any expansion model.

From the dimming analysis, we have estimated the mass and kinetic energy of the erupting CME, as well as the magnetic flux at the feet of expanding field lines. These measurements may set the lower-limits of relevant quantities of the CME. It is possible that a bulk of the CME is formed by reconnection within a pre-flare sheared arcade, whose flux and mass are entrained into the CME. If a major part of this arcade does not rise or expand rapidly before reconnection, dimming signatures would not be produced at the feet of these arcade field lines, and therefore the mass and flux involved in these structures would not be counted in the dimming analysis.

Admittedly, our analysis is subject to over-simplified assumptions. We have assumed that the expansion of coronal structures anchored at various dimming locations is approximated by or linearly scaled with a single CME height measured in the STEREO FOV, and a mean pre-eruption temperature is used for all dimming pixels. In reality, different regions may be subject to different physical conditions. Nevertheless, the observed timing relation among the flare, CME, and dimming, and the spatial pattern of dimming signatures can provide useful constraints to advanced models studying reconnection and eruption in solar corona. We also remark that gradual dimming is observed at some locations, starting about 30 minutes before the onset of the CME eruption and flare reconnection. It is plausible that this gradual and weak pre-eruption dimming may reflect the slow expansion of coronal structures, which can be further studied in search for early signatures of CMEs.

We thank the referee for constructive comments that helped improve the clarity of the paper. This work is supported by the NSFC under grants 11303073, 11373023, 11133004 and 11103008. This research is supported by the strategic priority research program of the Chinese Academy of Sciences (grant No. XDB09000000). This research is also supported by the open project of Key Laboratory of Solar Activity, National Astronomical Observatory, Chinese Academy of Sciences. The AIA data used here are courtesy of SDO (NASA) and the AIA consortium. STEREO is the third mission in NASA's Solar Terrestrial Probes program. The SECCHI data are produced by an international consortium of the NRL, LMSAL and NASA GSFC (USA), RAL and University of Birmingham (UK), MPS (Germany), CSL (Belgium), IOTA and IAS (France).

Footnotes

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10.3847/0004-637X/825/1/37