Section 1 Introduction
Solar flares are sudden brightenings occurring in the atmosphere of our Sun that can be monitored in a large range of the electromagnetic spectrum. They are associated with intense radiations, the release of energetic particles, as well as in some cases the ejection of solar plasma and magnetic field in the form of coronal mass ejections (hereafter, CMEs). As such, solar flares are major drivers of space weather (Gosling et al., 1991) as they can impact planetary environments (Prangé et al., 2004) and in particular human activities (Schrijver et al., 2014; Lugaz, 2015). Further away from our solar system, flares are also seen to occur on other stars (Linsky, 2000), as reported by the new findings from the NASA-Kepler mission (Walkowicz et al., 2011; Wichmann et al., 2014). Therefore, understanding the mechanisms of solar flares is important, not only to better predict the changes occurring in the Earth’s environment, but also to a large extent, to understand star-planet interactions. This will ultimately help to assess planetary habitability conditions (Poppenhaeger, 2014; Strugarek et al., 2014).
The first solar flare ever recorded was also one of the most powerful (although its energy content has been greatly debated, see McCracken et al. 2001; Tsurutani et al. 2003; Wolff et al. 2012; Cliver and Dietrich 2013). It occurred on 1 September 1859, as reported by Carrington and Hodgson (Carrington, 1859; Hodgson, 1859). To date, the flare of 4 November 2003 is the most energetic flare recorded with recent instrumentation. Its soft X-ray emission was above the X28 range. The existence of super-flares on other stars (Maehara et al., 2012) therefore requires investigating whether flares more intense than that observed so far can occur on our aging Sun (Schrijver et al., 2012; Aulanier et al., 2013). This question, linked with the dynamo evolution in the Sun’s interior, also requires a further understanding on how the energy of flares is stored, and what mechanisms can account for its release. Note that flares are seen to occur over a large range of the energy spectrum: small-scale flares, associated with rather low energy events (10 to 10J), are monitered in the quiet regions of the Sun. These so-called nanoflares or subflares will not be the focus of the present article.
With ever increasing spatial and temporal resolutions, instruments onboard more recent spacecraft now monitor the Sun in different wavelengths, providing detailed observations of the evolution of the photospheric, chromospheric and coronal plasma and magnetic field. They therefore provide strong constraints on models of solar flares. As such, understanding their mechanisms encompasses a variety of approaches, from deciphering the observational features to developing numerical models that capture their underlying physics. Dedicated reviews of solar flares are numerous: while some review the relevant physics to describe the magnetic conversion process during flares (see e.g. Priest and Forbes 2002; Shibata and Magara 2011), others report on the variety of their observational features (see e.g. Krucker et al. 2008; Fletcher et al. 2011). Although reviews on the models and simulations developed to explain flares are also available (e.g. Chen, 2011), they generally focus on a 2D or 2.5D description of the magnetic field in the solar atmosphere. To fill this gap, we present in the following sections a review of the recent modelling developments that incorporate the intrinsic, and therefore essentially 3D nature of solar flares. We will see the wealth of methods now developed to extrapolate the coronal magnetic field, to characterise 3D topological features, and to reproduce the dynamics of the field in 3D. The present review aims at explaining how these techniques and observations provide the building blocks to construct 3D models of solar flares. In particular, we propose in the final section how different features of eruptive flares can be combined to construct a comprehensive, yet rather complete, standard 3D model for eruptive flares.
Section 2 briefly reviews the observational characteristics of solar flares, with a particular focus on the differences between confined and eruptive flares. Section 3 reviews the current understanding of energy storage and introduces the concept of topology to understand where flare energy release is initiated. Section 4 discusses the evolution of flares, from their onset through their decline, and in Section 5 we focus on eruptive flares leading to the ejection of flux ropes and the characteristics of the 3D magnetic reconnection process. Finally, conclusions to this article are presented in Section 6.
Section 2 Observational Characteristics of Confined and Eruptive Flares
2.1 Flare Emissions
Flares are defined as impulsive releases of radiative energy over a large range of the electromagnetic spectrum (see Figure 1). The classification of flares is made with the soft X-ray, using the 1-8 Å band of the GOES-5 satellite (Geostationary Orbiting Environmental Satellites). This classification ranks flares from the A class to the X class (A,B,C,M,X), with the X class associated with the most energetic flares (with a GOES flux exceeding Wm at Earth, and the other classes decreasing by one order of magnitude). Weak events occurring at an energy level about times lower than large flares have been named “nanoflares”, and are being investigated as a possible mechanism for the heating of the corona (see Klimchuk and Bradshaw, 2014, and references therein), following the seminal idea of Parker (1988). In between, microflares, with energies of order times those of large flares, have been statistically investigated by Hannah et al. (2011). The authors, using the Reuven Ramaty High Energy Solar Spectroscopic Imager (RHESSI, Lin et al. 2002), showed that the physics that underly larger flare events can be extended down to smaller events. This is a remarkable outcome of the survey of flares and their emission within a large range of the electromagnetic spectrum. Indeed, the distribution of flare parameters, such as their estimated radiated energy, can be represented by a power law (see e.g. Figure 3 of Schrijver et al. 2012 and references in the paper).
A distinction can be made between confined and eruptive flaring events, a classification that was proposed already back in the 1980s by Svestka (1986). Confined flares are generally impulsive in time and compact in space, and the flare loops (see Section 2.2) contain most of the energy. They are accompanied by a population of accelerated particles and intense plasma radiation indicating that strong heating occurs. Eruptive flares, on the contrary, generally extend to a large volume of the corona and lead to the ejection of solar material in the form of coronal mass ejections. Although a distinction cannot be made between those two flare categories by only looking at the light curves, a coronagraph is generally a straightforward way to define them, as shown in Figure 2. Note that if eruptive flares are defined by the presence of a CME, the inverse is not true: CMEs have been seen leaving the solar atmosphere without an associated flare emission. These cases, referred to as stealth CMEs (see the review of Howard and Harrison, 2013, and references therein), can be associated with coronal phenomena invisible to present instruments, and therefore should be considered as a space weather prediction pitfall, as they are less well monitored.
Yashiro et al. (2005) investigated the link between CMEs and flares by associating events observed over a period of 7 years, and found that the CME association rate with the intensity of the flare increases from 20% for C-class flares (between C3 and C9 levels) to 100% for large flares (above the X3 level). However, X-class flares are not necessarily all associated with CMEs as the recent series of X-class flares of October 2014 in AR 12192 has shown (Thalmann et al. (2015), see also the studies by Feynman and Hundhausen 1994 and Green et al. 2002). This therefore leaves the question of the relation between intense flares and eruptiveness still open.
Both eruptive and confined events share some similarities in the evolution of the flare emission, as they are both characterized by an increase in radiation and are associated with emissions due to a population of non-thermal electrons, that is generally not detected in the non-flaring corona. However, eruptive flares are generally associated with long duration events, while confined flares typically have a much shorter time scale, as was shown in the study of Yashiro et al. (2006). The flare emissions for both type of events in different wavelengths do not peak at the same time (see also Fletcher et al., 2011, and references therein): typically, a brightening in soft X-rays of a few keV is first detected, associated with the chromospheric plasma heated to coronal temperatures. Also, radio emissions in the metric range, such as type III radio bursts caused by escaping electron beams, give an indication that the pre-flare phase is not entirely thermal. Most of the flare energy is then released during a short-span phase referred to as the impulsive phase, that is highly non-thermal. It is generally associated with hard X-ray emissions due to energetic electrons, as well as gamma-ray line emission caused by energetic ions. It is believed that most of the free coronal energy is released during this phase under the form of non-thermal particles, with electrons reaching energies up to 300 MeV, and ions up to 10 GeV. As the flare progresses during this phase, the soft X-ray emission increases in size and total flux, while the lower chromosphere also radiates more, as indicated by a growing H emission. After the impulsive phase the decay phase starts, where most of the emissions due to non-thermal particles have disappeared. The hot plasma decreases in temperature to the point that it also completely disappears, and flare loops, filled with evaporated dense plasma, emit in H.
2.2 Flare loops, Ribbons and Kernels
One of the most remarkable features of flares is the appearance of very hot coronal loops (T10 MK), referred to as flare loops, which remain above the flaring region (contrary to the CME during eruptive flares). Since they emit in different temperature ranges, it is possible to see their evolution in time with different filters. Looking at this evolution in just one filter is however misleading, as these loops would be seen growing in size (Figure 3a). However, following the same loop, it typically appears first in hot filters and progressively shifts to colder filters while it shrinks in height (Forbes and Acton, 1996). Moreover, newly formed loops are forming above already existing loops (e.g. Raftery et al., 2009; Sun et al., 2013).
Another characteristics of these flare loops is the evolution of their shear (Figure 3b). The shear angle is defined between the polarity inversion line (PIL) and the line that joins their footpoints, and as such, requires flares with a well-defined two-ribbon configuration and that are mostly observed near center-disk (so as to avoid any projection effects). This evolution was studied in various papers (Asai et al., 2003; Su et al., 2006; Aulanier, Janvier, and Schmieder, 2012), where conjugate footpoints at first indicated strongly sheared field lines, and later reveal less sheared coronal connections (Figure 3b). Su et al. (2007) also studied 50 X- and M-class flares observed with TRACE, associated with an arcade of flare loops, and found that 86% of these flares showed a general decrease in the shear angle.
The flare ribbons, discussed above, are intense emissions forming at the footpoints of flare loops, and are generally well seen before the appearance of the flare loops, mostly in H, but also in other EUV filters, as shown in Figure 3b,c. Flare ribbons appear in their fully developed state as coherent and elongated structures. They are frequently accompanied by spatially localised and strongly brightened clumps, referred to as kernels (Figure 3c). Because of their strong emission in chromospheric lines, it is believed that kernels and ribbons, form as a result of strong heating of the chromospheric plasma, most likely by collisions with non-thermal electrons. The evaporation of this strongly heated plasma can be seen as Doppler shifts in the diagnostics of spectral lines, for example with the EIS/HINODE instrument, as investigated by del Zanna et al. (2006), Milligan and Dennis (2009) and Young et al. (2013). Some parts of flare ribbons are also associated with the sites of HXR emissions (see Fletcher and Hudson 2001, Asai et al. 2002, Reid et al. 2012).
Eruptive flares generally display two ribbons with a large portion generally parallel to each other, and which also present a hook shape at their ends (Figure 3c, see also Chandra et al. 2009). It was shown, e.g. in Janvier et al. (2014), that this hook surrounds a dimming region generally associated with the footpoints of the ejected CME. For confined flares, flare ribbons can be more numerous (see for example Wang et al., 2014) or have different shapes (see for example a circular ribbon configuration in Masson et al., 2009). As such, the presence of two ribbons with a -shape structure is interpreted as an evidence of an eruptive flare.
2.3 Filaments/Prominences, and CMEs
Prominences, which appear on the limb as bright structures, or filaments, dark filamentary objects on disk, are potential progenitors of eruptive flares (Figure 4a). These structures, which are observationally complex to understand (see the recent reviews of Schmieder and Aulanier 2012; Engvold 2015 and accompanying references), are indeed often associated with CMEs (Figure 4b,c). This association has been thoroughly investigated in a series of papers (Subramanian and Dere 2001, see also the reviews of Schmieder, Malherbe, and Wu 2014 and Webb 2015). In particular, filaments/prominences eruptions and CMEs are generally well associated, from 56% to 92% of the former associated with CMEs (Hori and Culhane, 2002; Gopalswamy et al., 2003; Jing et al., 2004).
Note that some flares, which would be confined by definition (no CME observed), clearly show the beginning of a prominence or filament eruption, although instead of lifting off to greater altitude, the structure remains above the region. Such cases are generally called failed eruptions (see for example in Ji et al. 2003, Gilbert, Alexander, and Liu 2007 and Joshi et al. 2015).
In active regions, CME precursors are often seen as a bright structures made of or -shaped coronal loops, forming what is called a sigmoid (Rust and Kumar, 1996; Canfield, Hudson, and McKenzie, 1999; Green and Kliem, 2009). They are present with the filament (see the example in Figure 4a), and they are generally well seen in the X-ray range (see the catalogue of sigmoids in Savcheva et al. 2014).
Section 3 Energy Build-up and Release
The energy of a solar flare is typically estimated to be between to a few erg (see Schrijver et al., 2012). With a plasma , the magnetic field drives the coronal activity, and its associated energy is the only component that can account for flare power. Looking at the evolution of light curves (for example those of Figure 2), several questions arise: How to explain the long duration energy storage phase, lasting from a few days to a few weeks? What are the mechanisms for the sudden energy release? What triggers flares, and how is the energy converted into other types of energy (i.e., kinetic energy, radiation)? In the following, we review recent theoretical and numerical developments that try to answer these questions.
3.1 Mechanisms for Energy Build-up
For a given distribution of the normal component of a photospheric field, the potential field (current free) has the lowest magnetic energy. Any excess is called “free energy” and it is stored as currents in non-potential field configurations. Indeed, there is indirect observational evidence of strong electric currents stored in magnetic structures prior to an eruption onset. This is particularly the case with the X-ray emitting sigmoids, as investigated by e.g. Green et al. (2007); McKenzie and Canfield (2008); Savcheva et al. (2012a), and with the presence of twisted filaments/prominences (e.g. Williams et al., 2005; Koleva et al., 2012). How can such magnetic fields that store their energy in aligned currents be created?
Two mechanisms can account for the energy storage. One is the emergence of sub-photospheric current-carrying flux tubes from the convection zone (Figure 5, top row). Several authors have reported observational evidence that the Sun’s magnetic field is often twisted on emergence (Leka et al., 1996; van Driel-Gesztelyi, 1997; Luoni et al., 2011).
Numerical simulations are heavily used to study the photospheric emergence since the physical problem is complex (see the reviews by Fan, 2009; Hood, Archontis, and MacTaggart, 2012; Cheung and Isobe, 2014). This complexity is in particular linked to the presence of a large stratification of the plasma and magnetic field (since the scale height of the photosphere is only about 150 km). This implies that a flux rope coming from the convective zone is no longer buoyant below the photosphere. There, its magnetic field is blocked in a flat structure until enough magnetic flux has accumulated. This leads to the development of the so-called Parker instability, allowing the magnetic flux to emerge by pieces into the chromosphere and corona. As such, the magnetic field is completely changed from its initial state during this emergence, and finally it is a new flux rope that reforms in the corona (Hood et al., 2009; Toriumi and Yokoyama, 2012). In some simulations, the coronal flux rope is eventually ejected (e.g. Archontis and Hood, 2012; Kusano et al., 2012). However, the key parameters leading to such an ejection still remain to be understood (see Section 4).
Another mechanism that can account for the formation of a current-carrying magnetic field is slow photospheric motions, for example by twisting the polarities, or by inducing a shearing motion parallel to the inversion line. Moreover, flux ropes can form by reconnection of low field lines, such as in the model of van Ballegooijen and Martens (1989). This reconnection at the PIL occurs as the magnetic field diffuses gradually at the photosphere as found in numerical simulations (e.g. Amari et al., 2003b; Aulanier et al., 2010; Amari et al., 2011; Amari, Canou, and Aly, 2014). There, the presence of current density layers at bald patches (regions where the magnetic field is tangent to the photosphere) leads to the reconnection of magnetic field lines that create a newly formed structure made of twisted flux bundles, embedded in an overlying, almost potential arcade. High electric currents confined in this structure are similar to the - or -shaped sigmoids often observed in observations (see Figure 5, bottom row).
3.2 Reconnection: a Mechanism for Flares
As discussed in the previous section, magnetic reconnection is thought to be the key mechanism that permits the evolution of the field in the storage phase and the eruptive phase of flares. Already recognizing its importance back in the 1950s, Sweet (1958a) and Parker (1957) developed a theory, based on a work by Dungey (1953), that could explain how the magnetic energy contained in the corona could be released efficiently while giving the intense radiation recorded during flares. Such a mechanism is related to the fact that in an evolving magnetic configuration with a null point, a current sheet typically forms. This thin sheet introduces small scales where dissipative effects become important. In such a current sheet, the magnetic energy is dissipated into heat, kinetic energy and energetic particles. By applying this theory to solar flares, they defined a flaring configuration with four domains of connectivity. The reconnection of field lines between these regions converts magnetic energy into other forms of energy, while transforming the magnetic field configuration.
Since these pioneering works, there has been a tremendous number of studies on magnetic reconnection, especially in relation to flares, and the reader is referred to previous reviews (Forbes, 2010; Shibata and Magara, 2011; Priest, 2014, Chap. 12). Here, we only note that in 2D, i.e. in the presence of separatrices, which are special field lines separating different domains of connectivity, the definition of reconnection is clear. It can be defined both mathematically by a change of connectivity domain for some field lines, and physically by the dissipation of the magnetic energy within thin layers. A definition that is both mathematical and physical is an important distinction to make, as in 3D, mathematically well-defined separations of connectivity domains do not necessarily exist (see Section 3.4), while the reconnection, defined physically as the dissipation of magnetic energy in thin electric current layers, remains a valid concept.
There is much evidence that the reconnection process takes place in the corona. One aspect of it is the formation of a population of non-thermal particles, that is also observed in plasma experiments and in in-situ data of the magnetosphere (see chapter V.B in the review of Yamada, Kulsrud, and Ji 2010). For solar flares, several authors have reported on the existence of hard-X ray sources above the flare loop tops (e.g. Masuda et al., 1994; Hudson et al., 2001; Sui and Holman, 2003), indicative of a source forming high-energy particles (see Figure 6c). In particular, Masuda et al. (1994) proposed a heating process due to high speed jets produced by reconnection, colliding with the top of the reconnected flare loops. Furthermore, flare loops are ordered in temperature with the outermost loops being the hottest, as expected for a reconnection process that forms them sequentially at larger height (see e.g. Forbes and Acton, 1996; Tsuneta, 1996).
Another strong evidence that magnetic reconnection is taking place is given by the presence of inflows and outflows from and to the reconnection site. For example, as reported by Yokoyama et al. (2001), the authors used EUV and soft X-ray observations of a flare with the EIT/SOHO (Delaboudinière et al., 1995) and SXT/Yohkoh (Tsuneta et al., 1991) instruments, and pointed out the pulling process of coronal loops in a region underneath a plasmoid ejection and above the top of the flare loops (Figure 6a,b). Using diagnostics from the soft-X ray emissions, they were able to deduce an inflow speed. Outflows, on the other hand, are often seen as void structures in EUV and SXR emission ranges above flare loops. Sunward-flowing voids are referred to as supra-arcade downflows (SADs, see McKenzie (2011) and Figure 6f), propagating with a speed ranging from 50 to 500 km.s (sub-Alfvénic). They have been interpreted as coronal loop cross section evacuated from the reconnection region (Savage, McKenzie, and Reeves, 2012). Inversely, plasmoids ejected away from the Sun have also been reported (Nishizuka et al., 2010) in increasing numbers with the temporal and spatial capacity improvements of AIA onboard SDO (Takasao et al. (2012) and Figure 6d,e). Using radio emissions, more refined analysis of the dynamics of these plasmoids provides more insights on the reconnection mechanism at the origin of their ejection (e.g. Nishizuka et al., 2015). Finally, inflows and outflows are often seen together, as reported in the coronal observations of Yokoyama et al. (2001); Li and Zhang (2009); Savage et al. (2012); Takasao et al. (2012); Su et al. (2013).
When magnetic energy is released in the corona, a significant part of this energy is also transported along field lines by thermal conduction fronts, and/or energetic particles, and/or Poynting flux (e.g. Fletcher and Hudson 2008, Birn et al. 2009, Longcope and Tarr 2012) toward the lower atmosphere. This generally makes the first energy release of flares (see Krucker, Fivian, and Lin, 2005; Saint-Hilaire and Benz, 2005, and references therein). Then, the chromospheric plasma becomes hot (up to tens of millions of degrees, as seen in soft X-rays), as non-thermal particles collide with the particles of this atmospheric layer. Intense radiation can be seen as hard X-ray sources at the footpoints of bright flare loops, which used to be referred to as post-flare loops, (e.g. kernels, see Section 2.2), but also at the footpoints of twisted loops, as reported by Liu and Alexander (2009) and Guo et al. (2012). Note that for both cases, HXR sources were found at the endpoints of the associated filaments, appearing during a failed eruption. Eruptive flares do not usually show such intense emissions, although it is possible to find such cases (Musset, Vilmer, and Bommier, 2015). As the chromosphere expands, evaporation of hot plasma ensues, filling up coronal loops that are then seen as flare loops (see Section 2.2). Much of the energy coming from the non-thermal population is eventually converted into thermal energy and radiation, seen dominantly as the UV and optical component of the flare (see e.g. Milligan et al., 2014). Therefore, measuring the radiative losses of flares is almost equivalent to the flare’s energy release. Almost, since one would also need to measure the bulk kinetic energy from the ejecta and the escaping particle populations to obtain an accurate description of the total energy of a flare.
3.3 Using Topology to Find Reconnection Regions
In order to localize where reconnection could occur, one needs to search for the regions where the evolving magnetic field can form current layers, in other words, where ideal MHD breaks down. These regions are found by analyzing the magnetic topology of the field.
The first models of reconnection were 2D. In 2D, the magnetic field can be separated in different domains of connectivity by special field lines that are called separatrices. Two separatrices cross at a null point, where the magnetic field vanishes (Sweet, 1958b). From the 1990s, a great deal of work has been made with extensions of those mathematically defined features from 2D to 3D. Separatrices in 3D are surfaces, which delimit different domains of connectivity. The intersection of two separatrices defines a separator, which is a privileged location for reconnection to occur. It is a special field line joining two null points. The complete topology description of a magnetic field is given by the skeleton formed by null points, separators and separatrices. Reconnection taking place at each of these topological features in 3D has been at the core of several works which explored the complexity of possible magnetic topologies (e.g. Longcope and Cowley, 1996; Parnell et al., 1996; Priest and Titov, 1996; Pontin, Hornig, and Priest, 2004, 2005; Pontin, Bhattacharjee, and Galsgaard, 2007; Priest and Pontin, 2009; Parnell, Haynes, and Galsgaard, 2010, and references therein).
The application of the above theory to solar flares started to be developed around the 1980s by placing a few magnetic sources below the photosphere, so as to reproduce the observed magnetograms. The topology is then computed and compared to flare observations (Baum and Bratenahl, 1980; Gorbachev and Somov, 1988; Lau, 1993). The complexity of the model was later increased to include many more sources with positions and strengths being computed by a least square fit of the model to the magnetogram of a specific observation. This procedure defines the coronal magnetic field and its topology (via magnetic connectivity between magnetic sources). Several flare studies found that the observed flare ribbons are located in the vicinity of the computed separatrices. This is evidence that the energy release occurs by magnetic reconnection (e.g. Mandrini et al., 1993; Démoulin et al., 1994).
This approach was further developed in the so-called Magnetic Charge Topology (MCT) model (e.g. Barnes, Longcope, and Leka, 2005; Longcope, 2005), in particular by estimating the amount of electric current flowing along the separator before reconnection and the amount of reconnected flux during the observed flare. Although successful in describing reconnection signatures for a variety of solar active regions, the MCT model is limited since it requires one to first split the observed magnetogram into a series of separated polarities, which is ambiguous for unipolar regions. The topology is computed as if every polarity, modeled by a charge, is surrounded by flux free regions. The above approach introduces an ensemble of null points and separatrices that are not all in the coronal field computed from the photospheric magnetogram using force-free extrapolation methods.
3.4 Quasi-Separatrix Layers
Flares with comparable characteristics are observed with and without magnetic null points and their associated separatrices (Démoulin, Hénoux, and Mandrini, 1994). Therefore, extending the concept of separatrices to regions where the magnetic field connectivity remains continuous but changes with a strong gradient,Démoulin et al. (1996) introduced the concept of quasi-separatrix layers (QSLs). These are mathematically defined with the Jacobi matrix of connectivity transformation from a photospheric positive polarity domain to a negative polarity domain, or simply put, by the field line mapping of the magnetic field. Regions where the magnetic field is strongly distorted, or “squashed”, are defined by a strong value of the squashing degree (Titov, Hornig, and Démoulin, 2002; Pariat and Démoulin, 2012). As such, computing QSLs allows the magnetic topology of an active region to be defined when the coronal configuration is computed by any means (e.g. magnetic extrapolation or MHD simulation).
QSLs are a generalisation in 3D of the concept of separatrices. In the limit where photospheric unipolar regions are separated by flux-free regions, or when a magnetic null enters in the coronal domain, or when a pair of nulls appears after a bifurcation, the central parts of QSLs become separatrices (Démoulin et al., 1996; Restante, Aulanier, and Parnell, 2009). QSLs with large values still remain on both side of a separatrix (where becomes infinite, Masson et al., 2009). Finally, because of the strong distortion of the magnetic field, strong current density build-up typically occurs at QSLs during the magnetic field evolution (as shown in Aulanier, Pariat, and Démoulin 2005; Büchner 2006; Effenberger et al. 2011; Janvier et al. 2013). As such, QSLs are preferential locations for reconnection to take place. This was evidenced observationally by the correspondence between flare ribbons and QSL locations and by the presence of concentrated electric currents located at the border of the QSLs (Démoulin et al., 1997; Mandrini et al., 1997).
Hesse and Schindler (1988) and Schindler, Hesse, and Birn (1988) developed a general framework for 3D reconnection in the absence of null point and separatrices. Their formulation of the magnetic field with Euler potentials allows the description of the evolution of field lines and to pinpoint how and where they are cut, therefore accessing the physics of 3D reconnection. It occurs where localised non-ideal regions are set. QSLs are the locations where these non-idealness can occur as strong current density typically build there during an evolution. Therefore, the two approaches are complementary, with the QSLs providing the large scale topology, localising where reconnection occurs, and the formalism of Hesse and Schindler describing the local reconnection process within the MHD framework (Démoulin, Priest, and Lonie, 1996; Richardson and Finn, 2012). These results were recently extended to kinetic numerical simulations (Wendel et al., 2013; Finn et al., 2014).
The QSL theory has been tested in several simple configurations, for example in cases where two interacting bipoles in a solar active region could be easily identified (Démoulin et al., 1997). The theory has also been extensively used to understand more complex cases. A sample of the many other studies looking at the location of reconnection signatures, typically flare ribbons, and comparing them successfully with the locations of QSLs, can be found in Schmieder et al. (1997); Bagalá et al. (2000); Wang et al. (2000); Masson et al. (2009); Chandra et al. (2011); Savcheva et al. (2012b); Zhao et al. (2014); Dudík et al. (2014); Dalmasse et al. (2015). This close correspondence between flare ribbons and separatrix/QSLs found in various magnetic configurations, and derived from the photospheric magnetograms, is strong evidence that magnetic reconnection is releasing the free magnetic energy in flares.
In the above flare applications, computing QSLs in a magnetic field volume is more demanding of computer ressources than locating the null points in the MCT model, due to the large amount of field lines to process. The advantage of the QSL method is that it can be applied to any magnetic extrapolation technique, and with any theoretical model (for example see Section 5.1). Furthermore, the calculation of QSLs can be sped up with the use of a refinement algorithm using an adaptive grid that progressively computes field lines only where the thin QSLs are located (Démoulin et al., 1996; Pariat and Démoulin, 2012).
Section 4 Magnetic Environment of Flares
4.1 Confined Flares: Emerging Flux
A model for emerging flux and energy dissipation was proposed by Heyvaerts, Priest, and Rust (1977) then Forbes and Priest (1984) for confined flares: as new flux emerges from the photosphere, it presses against overlying field structures, leading to the formation of a current density layer. As this process goes on, the current in the sheet grows, until a critical threshold is reached and triggers a micro-instability. The occurence of such an instability can lead to an increase in the local resistivity of the plasma, which in turn can rapidly dissipate the current (see Section 3.2). Then, not only is flux emergence associated with the transfer of current-carrying magnetic field structures (see Section 3.1) from the solar convection zone to the atmosphere, it can also account for triggering energy releases by forcing the transformation of the magnetic field configuration.
On the other hand, large scale flux emergence can also occur with the appearance of new polarities emerging in older regions, without being necessarily associated with an already formed flux rope. Such conditions then lead to the appearance of several magnetic field connectivity domains. For example, several examples (e.g. Mandrini et al., 1993; Gaizauskas et al., 1998) showed that almost oppositely oriented bipole that emerged between the two main polarities of an AR created topological conditions for current layers to form, and as such for flaring activity to occur. In particular, in the active region 2372 studied by Mandrini et al. (1993), some of the H flaring kernels were directly associated with flux emerging processes. Therefore, the appearance of several domains of connectivity, as well as their associated photospheric motions, are both favorable conditions for magnetic reconnection to take place. Since flux emergence is ubiquitous and continuously takes place in the solar corona (Schrijver, 2009), this mechanism has been put forward as possibly an important process occurring in the majority of flares, and is in particular a rather straightforward process to trigger confined flares.
A test of flux emergence as a possible mechanism for confined flares as been proposed as follows. Masson et al. (2009) studied an important emergence occurring in the middle of AR 10191 and which led to a confined flare on 16/11/2002 (SOL2002-11-16T13:58). The photospheric motions are first modeled to reproduce the evolution of photospheric magnetograms from MDI/SOHO (Scherrer et al., 1995), and a potential magnetic field extrapolation is used as an initial condition. The MHD evolution shows the build up of localized electric currents, then the release of magnetic energy by reconnection. This magnetic reconnection takes place at the null point and the surrounding QSLs, and leads to the formation of newly reconnected field lines (Figure 7b,c) in good correspondence with coronal observations (Masson et al., 2009). Note that although the simulation was defined as a case study for AR 10191, similar configurations of reconnected field lines can be found in other confined flares and now in other data-driven simulations of null-point reconnection. Figure 7d,e represents heated coronal loops before and after the 11/03/2014 (SOL2014-03-11T03:50) flare event obtain with the AIA instrument onboard SDO, and is presented as an illustration.
4.2 Eruptive flares: Unstable Flux Ropes
Since eruptive flares are defined as CME-accompanying flares, there is a necessity to understand what triggers its magnetic field configuration to be ejected in the first place. Since this structure can remain stable from days to weeks above the solar surface (see prominences/filaments in Section 2.3), a CME ejection can be seen as a sudden loss of balance between two acting forces: the magnetic tension of coronal arcades above the flux rope that pushes it downward, and the magnetic pressure of the flux rope that leads to further expansion. Then, a search for a trigger mechanism must account for either the magnetic tension to reduce or for the magnetic pressure to increase. In the review of Aulanier (2014), the author discussed the necessary ingredients for a twisted structure to be expelled in the outer corona, which we briefly recall in the following.
Looking at the evolution of active regions or regions associated with prominences and filaments can help understand what the ingredients to be accounted for triggering scenarios are. For example, during the decaying phase of active regions the dispersion of magnetic flux by convective motions implies a converging motion at the PIL as well as flux cancellation. (e.g. Martin, Livi, and Wang, 1985; Schmieder et al., 2008; Green, Kliem, and Wallace, 2011). The coronal response to such photospheric evolution has been studied in many numerical models, such as the 3D simulations of Amari et al. (2003a), Mackay and van Ballegooijen (2006), Yeates and Mackay (2009), and Amari et al. (2011,2014). While flux cancellation at the PIL leads to magnetic flux decrease in the photosphere, it transforms the magnetic arcades overlying the flux rope - in other words, the overlapping field lines, to field lines wrapping around this flux rope, so further building it. Then, the photospheric evolution leads to a decrease in the coronal magnetic tension, a favorable condition to weaken the downward force acting on the flux rope.
Although several other processes can be identified as participating in the triggering processes (such as small and large scale reconnection inducing tension weakening, flare reconnection from below, shearing motions building up pressure below the overlying arcades, flux cancellation decreasing the arcade flux – see references in Aulanier 2014), a question remains about the actual intrinsic mechanism that triggers flares. Such a model would take into account the different phenomena observed prior to flares, explaining the trigger of CME eruptions for a majority of the cases. Then, several authors have studied flux rope ejections with numerical simulations by bringing a flux rope to an unstable state (Figure 8): Amari et al. (2000); Lin, Forbes, and Isenberg (2001); Forbes et al. (2006); Fan and Gibson (2007); Aulanier et al. (2010); Olmedo and Zhang (2010); Zuccarello, Meliani, and Poedts (2012). The characterisation of this instability was proposed by Aulanier et al. (2010): from the formation of the flux rope (see Section 3.1), they studied its stability by turning down the driving forces (i.e. the photospheric boundary motions) at different times in the simulation. By doing so, they found that there is a threshold provided by the configuration of the flux rope, from which it becomes unstable. This instability is the torus instability (see also Kliem and Török 2006).
Another scenario has been proposed for the magnetic tension reduction by Antiochos, DeVore, and Klimchuk (1999) and DeVore and Antiochos (2008). In their so-called breakout model, a current sheet is formed in a quadrupolar configuration at the null point located above a sheared magnetic field configuration (which could also host a flux rope, but not necessarily). ÊAt some point of the evolution a fast reconnection is triggered there. It removes rapidly part of the magnetic tension over the sheared arcade, inducing its eruption. Although this configuration can be observed in the solar atmosphere (see e.g. Aulanier et al. 2000), it requires that too much flux cannot accumulate at higher altitude, otherwise the magnetic tension reduction via reconnection becomes too inefficient to account for the sudden ejection of CMEs. Since this scenario involves mostly sheared arcades rather than a flux rope structure, a main ingredient in the ejection of CMEs, we will focus in the following on simulations of torus-unstable flux ropes.
Section 5 Advances in flare QSL reconnection
5.1 QSLs in the Presence of Twisted Flux Tubes
It is necessary to understand the 3D topological features associated with flux ropes to explain the underlying processes linked to their ejection during an eruptive flare. In the analytical work of Démoulin, Priest, and Lonie (1996), it was shown that QSLs form a thin volume wrapping around flux tubes. Their mapping, down at the photospheric boundary, is representative of the twisted shape of the flux rope, with the hook part swirling more with a more twisted configuration (see Figure 9a,b). The evolution of QSLs during the formation of a flux rope by kinematic emergence through the photospheric boundary was investigated in Titov and Démoulin (1999). In particular, it was shown that as the flux rope fully emerges, the photospheric footprints of the QSLs split into two distinct traces, reminiscent of the H ribbons during flares (Titov, 2007).
This analytical flux rope (see Section 2 in Titov and Démoulin 1999) was reproduced numerically by Savcheva et al. (2012b) for comparisons with MHD simulations and observations. The volume associated with the highest values of the squashing degree (see Section 3.4), defined as the hyperbolic flux tube (HFT, Titov, Hornig, and Démoulin, 2002), is located below the flux rope (see Figure 9c). This HFT volume maps all the way down to the photosphere to the beginning of the hook-shaped structure (see the red area in the photospheric footprints of the QSLs in Figure 9d). In the close vicinity of the HFT, different types of connectivities are present. Above are field lines from the flux rope, below are arcade-like field lines, and on the sides are large scale arcade-like field lines surrounding the flux rope. This variety of connectivities in a small region implies that the QSLs, and especially their core, the HFT, are privileged regions both for current layer build-up and for the occurence of magnetic reconnection.
For configurations before eruptions, seen as on-disk sigmoid structures, it is interesting to compute the QSLs and this first requires to compute the coronal magnetic field. One of the most successful methods to reproduce the presence of a twisted coronal magnetic structure is that of van Ballegooijen (2004), who proposed inserting a flux rope in the magnetic region of a sigmoid region, extrapolated with a potential field, and leaving the system to relax using a magneto-frictional code. This method was successfully applied to several active regions presenting sigmoids as an evidence of the presence of a flux rope (Savcheva and van Ballegooijen, 2009; Savcheva et al., 2012b; Su and van Ballegooijen, 2012). In particular, in Savcheva et al. (2012b), the authors calculated the QSLs from their extrapolation method. As shown in Figure 9g,h, the structure of the QSLs, although more complicated due to the presence of more complex surrounding coronal loops, also show an HFT, tear-drop and cusp shapes above and beneath it, as well as hook-shaped photospheric signatures. As such, the presence of an HFT is an essential part in the sigmoidal structures seen in the corona, and as will be seen below, holds the keys to the underlying reconnection processes forming flaring structures.
From the results of the pre-eruptive magnetic field, one can predict that the flare reconnection will occur at the HFT. This analytical result was indeed verified in a dynamical MHD model reproducing the ejection of an unstable flux rope (Janvier et al., 2013), from the original setting of Aulanier et al. (2010) but with no photospheric boundary driving applied. Computing the squashing degree in the 3D volume, the QSLs are seen to wrap around the modeled flux rope (Figure 9e) similarly as the analytical flux rope model. As time evolves, the tear-drop shape becomes bigger as the flux rope extends, and the HFT underneath it moves upward, following the ejection motion of the flux rope, while the cusp region becomes wider. Since this cusp structure indicates the delimitation between the regions where field line have not reconnected (coronal field lines) and regions of reconnected field lines (the flux rope above the cusp, and the flare loops inside the cusp region), the cusp becomes wider as more flare loops are fed into the region.
The photospheric signatures of the QSLs, as seen in Figure 9f, also present a hook-shape structure, and the straight parts near the PIL move away from each other as the eruption goes on, while the hooks become rounder. Note that the hooks do not close onto themselves, as found in the analytical Titov-Démoulin model shown in Figure 9c,d. This is because the flux rope structure is not as twisted as that in the analytical model. A comparison with the morphology of the flare ribbons (see Section 5.3) indicate that flux ropes in the corona should not have twist much larger than one turn, contrary to what is suggested in kink-unstable flux rope models (Janvier et al., 2014).
5.2 Reconnection in 3D: Slipping Motion
Quasi-separatrix layers indicate regions of strong magnetic field distortion. When field lines are reconnecting with their neighbouring field lines in a QSL, their motion is seen as an apparent flipping, or slipping motion of field lines. This was analytically predicted by several authors (Priest and Forbes, 1992; Priest and Démoulin, 1995; Démoulin et al., 1996).
Since it is impossible to follow elementary flux tubes in the corona, numerical simulations present an invaluable resource to study the dynamics of field lines during the reconnection process. Indeed, by fixing a field line starting point, one can evaluate its successive changes of connectivity by tracing the line from its defined point, as time goes by. Note that if the change of connectivity occurs at super-Alfvénic time scales, the apparent slipping motion is said to be “slip-running” (Aulanier et al., 2006). This term refers to the fact that within the MHD paradigm information only travels up to the Alfvén speed in a low- plasma. The fixed footpoint of the magnetic field line at one end does not actually “see” the change of connectivity if its opposite footpoint moves at super-Alfvénic speeds this opposite footpoint is defined as the photospheric endpoint location of the same field line computed from the fixed footpoint location, . At the scale of the system, for super-Alfvénic or slip-running motion, field lines behave as if they had reconnected in the presence of separatrices. This motion has been reported in different simulation setups (Török et al., 2009; Masson et al., 2009, 2012; Janvier et al., 2013).
The characteristics of the slipping motion of field lines during an eruptive flare were studied by Janvier et al. (2013), and in particular the speed of the motion was quantified, for the flux rope ejection simulation shown in the bottom row of Figure 8. An example of a slipping field line is presented in Figure 10 (panels a and b), where the same field line, defined by its footpoint anchored in the negative polarity, is traced at different times in the simulation. Since the location of other footpoint is moving as the consequence of the field line reconnecting with its neighbouring field line, it is possible to report for each time step the distance travelled (Figure 10c, where the photospheric QSL footprints have also been reported), and hence the slipping motion speed, that is shown in Figure 10e. This slipping motion speed is not constant in time: rather, it has spikes, and its values can be sub- or super-Alfvénic.
As the location of the non-fixed footpoint moves along the QSL in the positive polarity, the other fixed point remains at the same location in the negative polarity. It is anchored outside of the QSL before the reconnection takes place, as indicated in the zoomed region in Figure 10d. However, as time evolves, this QSL moves away from the PIL, and hence “sweeps” the field line footpoint location. Indeed, as the flux rope is ejected away, the trailing reconnecting region moves upward, so that field lines passing through it reconnect with each other and the photospheric footprints of the QSLs in each polarity are then seen to move away from each other (similar to the CSHKP model, Carmichael, 1964; Sturrock, 1966; Hirayama, 1974; Kopp and Pneuman, 1976). As such, while the motion of the footpoint location in the positive polarity is along the QSL, the footpoint location in the negative polarity has a relative motion with respect to the QSL perpendicular to it. Then, the speed of the moving footpoint location is super-Alfvénic when the fixed footpoint is in the core of the QSL, and sub-Alfvénic on both sides. Note that taking a field line that would be defined by a fixed footpoint location in the positive polarity would give the inverse result: the fixed footpoint would move perpendicularly with respect to the QSL footprint in the positive polarity, while its corresponding displaced footpoint location in the negative polarity would move along the QSL footprint. Then, the slipping speed of the moving footpoint location is directly related to the distortion of the magnetic field, given by the field line mapping (, see Eq.(4) in Démoulin et al. 1996) and the speed at which the QSL is displaced: (see Janvier et al. 2013).
From its first prediction in the 1990s (Priest and Forbes, 1992; Priest and Démoulin, 1995; Démoulin et al., 1996) and its numerical modelling (Aulanier, Pariat, and Démoulin, 2005; Török et al., 2009; Masson et al., 2009; Janvier et al., 2013), the slipping motion of field lines has been observed for the first time in coronal loops (Aulanier et al., 2007) and during eruptive flares (Sun et al., 2013; Dudík et al., 2014; Li and Zhang, 2014) very recently. These observations, at high temporal cadence, can only provide evidence of sub-Alfvénic motions, since it is the only regime for which the response of the plasma to the change of connectivity can be observed. The slipping field lines of the coronal loops (Aulanier et al., 2007) was monitored with the XRT instrument onboard HINODE, and were seen to exchange their footpoint positions with a motion speed estimated between the 30 to 150 km/s. Dudík et al. (2014) reported the slipping motion of field lines in the X-class eruptive 1 July 2012 (SOL2012-07-12T16:50) with the AIA/SDO instrument, and also showed the propagation of kernel brightenings along the flare ribbons, reminiscent of the motion of footpoints obtained in the MHD simulation of a similar-looking active region (Janvier et al., 2013). The authors reported on apparent velocities ranging from 4 km/s to 140 km/s, and the successive kernel brightenings were associated with the footpoints of the field lines forming the envelope of the flux rope that eventually gets ejected during the flare (a CME was indeed recorded for this event). Note that since this process should be in principle intrinsic to any flare (as they all have a 3D structure), it is not related to the particular zipping brightening motion reported in some flares (Tripathi, Isobe, and Mason, 2006). The latter can be explained by the propagation of the reconnection site in one direction due to an asymmetric filament eruption, in which case both slipping motion and zipping motion can take place, although not necessarily on the same timescales.
5.3 Electric Current Evolution
The formation of electric current layers is an essential component of flaring activity. These thin layers are predicted to form in the regions where the magnetic field is strongly distorted, i.e. at similar locations as the Quasi-Separatrix Layers (see Section 3.4). On the other hand, as shown in Figure 9, QSLs form a coronal volume that maps all the way down to the photospheric boundary, with a photospheric signature presenting a -shape. Such a structure can be described in a 3D model of eruptive flares, where the core of the CME (i.e., the flux rope) fills a coronal volume embedded in the QSLs (see Figure 9) mapping in the hooks of the QSL footprints, flare loops are embedded in the cusp region, and field lines are slipping within the QSL. The representation of such a model is given in Figure 11, panel a, where these main characteristics have been put together. Then, do current layers have a similar morphology as that of the QSLs?
3D numerical modelling of eruptive flares has been able to answer this question by mapping the regions of high current densities. For example, in Kliem et al. (2013), the authors used an extrapolated field of the AR 11060 as an initial condition to run their numerical code. The associated 3D current layer for the present model, obtained as a current density itself derived from the components of magnetic field obtained in the simulation, is shown in Figure 11b. It presents a similar morphology as for the QSLs, although the high current density layer does not wrap around the flux rope as the QSLs do. This 3D view also shows the rounded hooks that surround the core region of the flux rope. In Janvier et al. (2013), the authors studied the evolution of the current layer as time goes by: a 2D cut in the central part of the flux rope 3D volume clearly shows the cusp region as well as the current layer above it where reconnection takes place. Note however that the region of highest density, found at the cusp in the 2D cut, is slightly offset compared with the location of the highest squashing factor location, namely the HFT (see Figure 2 of Janvier et al. 2013 for comparisons). As the flux rope expands, this current layer moves upward and becomes thinner, while the hooks of the photospheric current layers (shown for example in Figure 11f) become rounder and the straight parts of each current “ribbon” separate from each other, away from the PIL, as more flux is fed into the flux rope structure. As such, the 3D view contains the evolution of the field as represented by the 2D model. These modelled photospheric changes in electric current resemble those of observed bright flare ribbons during eruptive flares (e.g. Figure 11d). As such, the model for eruptive flares shown in Figure 11a incorporates the different evolution ingredients above. It proposes a development from the 2D point of view of the standard model of eruptive flares in 2D (or CSHKP model) to its more complete and more accurate 3D version (see Janvier et al., 2014).
A question that remains to be answered from the description above is how the flare ribbons and simulated photospheric current ribbons are related. Using the measurements of the three components of the magnetic field at the solar surface means that it is possible to observe the evolution of the photospheric current density, provided that there is a good spatial and temporal resolution. The HMI instrument onboard the Solar Dynamics Observatory has an unprecedented temporal resolution, providing maps of the line-of-sight measurements of the magnetic field every 12 mn. In Janvier et al. (2014), the authors used the Milne-Eddington inversion code UNNOFIT (see Bommier et al., 2007) applied to the HMI magnetograms covering the active region NOAAA 11158 during 4 hours of observation, including the X2.2 flare that took place on 15 February 2011 (SOL2011-02-15T01:56) and peaking at 01:56 UT. From this inversion process, maps of the vertical component of the current density vector were deduced. Note that although the active region presents a quadrupolar configuration, the X-class flare of Feb. 2011 was mainly confined within the two central bipoles, and as such had a configuration (including the asymmetry in the strength of the magnetic polarities) similar to that studied previously in the eruptive flare model of Aulanier, Janvier, and Schmieder (2012).
Investigating the evolution of at different times before and after the peak of the flare, the authors reported an increase in the direct electric current component along both the current ribbons in the negative and positive polarities (in regions indicated with arrows in Figure 11e). These current ribbons delimitate the region around the PIL where the magnetic field becomes more and more horizontal, showing that these regions do correspond to the formation of new post-flare loops (Sun et al., 2012; Wang et al., 2012; Petrie, 2013).
These results seem a priori contradictory to the core idea that flares typically dissipate the stored free energy as the magnetic configuration evolves toward a more potential, and hence less current-carrying, one. While a strong dissipation of magnetic energy is expected in the thin current layers, at the same time the electric current density increases due to the collapse of the thin layers. Such an evolution is due to the upward ejective motion of the torus-unstable magnetic flux rope: The field lines underneath the flux rope get squashed in the trailing current region (Figure 11c), which in turn thins while the current density increases there. Since this current volume maps all the way down to the photosphere (panel b), changes are then also expected to be seen at the photospheric level, as predicted in the numerical simulation (panel f). So although this mechanism competes with the strong diffusion taking place, the total current density is large at the beginning, during the flare impulsive phase, before decreasing later on.
The location and the evolution of enhanced electric currents within flare ribbons, predicted with numerical simulations, have now been confirmed thanks to the enhanced temporal and spatial resolution of recent instruments. They are not only correlated to the evolution of flare ribbons, as summarised above, but also to a variety of other phenomena: they map at similar locations as strong twist of the magnetic field, as shown in a data-driven simulation of the same X2.2 flare of 15 February 2011 (SOL2011-02-15T01:56) by Inoue et al. (2014), and regions of current changes have also been associated with HXR sources observed with RHESSI (Musset, Vilmer, and Bommier, 2015) as well as sunquakes (Zharkov et al., 2011).
Section 6 Conclusion
The present paper summarizes the MHD building blocks of solar flare modelling, from the topology to the trigger mechanisms, and from observations to 3D numerical simulations. While a flare is typically classified by its strength depending on its soft X-ray emission, it can also be differentiated in two categories, either confined or eruptive (see Section 2). While confined flares do not have a large influence on the global corona, eruptive flares are typically associated with coronal mass ejections (CMEs, see Section 2.3), and can therefore be potentially disruptive for surrounding planetary environments. They share similar features, such as the existence of ribbons and flare loops (Section 2.2).
Observations of solar flares inevitably lead to the question of the storage and the release of the magnetic energy that fuels them. Several mechanisms have been proposed (Section 3): one scenario involves current-carrying magnetic structures that form underneath the photospheric boundary, in the convection zone, and that are transported all the way to the corona. 3D simulations that have been developed recently are able to reproduce this emergence process, sometimes all the way to the ejection of current-carrying structures such as flux ropes (see Section 3.1). Other scenarios involve the formation of non-potential fields by photospheric motions such as shearing or flux cancellation, and have been tested against observations of the evolution of active regions and coronal loops.
Magnetic reconnection has been proposed as a mechanism to dissipate the free energy (Section 3.2). This phenomenon involves the creation of thin layers of high current density where the plasma becomes non-ideal, and where the magnetic energy can be converted into heat and kinetic energy, whilst forming a population of non-thermal particles. Although the spatial scales at which reconnection is expected to occur are too small for the present-day instruments to detect, its consequences have been witnessed in numerous cases, with an ever-increasing resolution (both temporal and spatial, Figure 6) over the years, and support the present theory. The regions of non-idealness can be found by searching for the topological characteristics of the magnetic field, such as the presence of null points, separatrices, separators, and also Quasi-Separatrix Layers (see Section 3.3). Current density layers, where the magnetic energy is dissipated, preferentially form at QSLs. Searching them in coronal magnetic fields has become a powerful and successful tool to understand the signatures of flare evolutions.
Using observations as well as numerical simulations, several major mechanisms can account for confined and eruptive flares. Emerging flux (Section 4.1) may possibly account for a great number of confined flares, although further understanding of the process driving them is required. Data-driven MHD numerical simulations can indeed explain such flares. Other observations of active regions have shown that several features appear prior to the onset of an eruptive flare, such as flux cancellation and flux dispersal, as well as shearing motions of the polarities. These mechanisms can provide the conditions for a flux rope to be formed. As discussed in the review by Aulanier (2014), those conditions can ultimately lead to a flux rope ejection via the torus-unstable flux rope model (Section 4.2). Next, we saw how the QSLs fill a thin coronal volume that maps all the way to the photosphere in the presence of a flux rope (Section 5.1). In their presence, the magnetic field lines change their connectivity successively, they are said to be slipping as time goes by (Section 5.2). This motion, first proposed as an analytical by-product of the presence of QSLs, has been investigated in detail in the numerical simulation of a flux rope ejection (Janvier et al., 2013). The slipping motion of field lines is intrinsic to the reconnection in 3D, and therefore, to all flares. Apparent motions of field lines and their associated kernels indeed have been observed with high-temporal resolution imaging.
Magnetic reconnection dissipates the magnetic energy in highly localised regions of high-current density, at the QSLs. Using numerical simulations of flux rope ejection, different study show a similar behavior and geometry: the coronal current layer where reconnection takes place form a volume that maps to the photosphere, following the QSL mapping. The impulsive phase of an eruptive flare is then dictated by the sudden thinning of the layer, where the electric current density increases, allowing reconnection to take place on a short time scale. This change of regimes has been confirmed by direct measurements of the photospheric vertical currents, with a high temporal-cadence instrument such as the HMI onboard SDO. This underlines the importance of using numerical models as they can also pinpoint consequences of such mechanisms that remain difficult to observe. They therefore provide the physical understanding to interpret observations, as well as the ideas for where and how to look at them. Taking into account the latest developments of numerical flare modelling, we report in Figure 11, panel a, on the extension of a 3D flare model from the previous CSHKP cartoon that remains valid only in 2D.
As discussed in the paper, MHD simulations of flares have been able to reproduce observational features, help to interpret the underlying mechanisms, and make predictions. Nonetheless, several issues still remain to be addressed, with further developments needed in the future. Indeed, within the MHD framework, the kinetic physics of the magnetic energy dissipation within the 3D current layer cannot be addressed. The length scales that account for this dissipation (the ion or electron length scales) are several orders of magnitude smaller than the typical lengthscale of coronal loops. As such, approximating the physics that takes place within the current layer (such as turbulence processes, plasmoid formation, Hall effect, ion heating, kinetic effects) is one solution, given the computer power available as of today, along with the development of hybrid codes. This also means that the MHD framework needs to be extended, so as to explain how a population of non-thermal particles is created. Recent developments in laboratory plasma physics, and in particular of the partition of energy between the different species (Yamada et al., 2014) may shed light on the processes happening in the corona. Furthermore, knowing the energy partition given to non-thermal particles is of high importance to understand how the energy is deposited from the corona to the photosphere (Milligan et al., 2014).
In conclusion, the correspondences between the 3D MHD models developed in the recent years, and the observations obtained with an increasing time and spatial resolution, provide strong evidence that several physical ingredients important to flares are included. Such models are of great importance not only to understand the flaring activity of our hosting star, but also to interpret data of other flaring stars, for which observations remain limited.
M.J. acknowledges partial funding from the SOC of the “Solar and stellar flares: observations, simulations and synergies” conference, held from 23-27 June 2014, where this work was presented. The authors would like to thank the anonymous referee and Lyndsay Fletcher for their useful comments that helped improve the article.
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