Magnetohydrodynamics modeling of coronal magnetic field and solar eruptions based on the photospheric magnetic field

Satoshi Inoue

doi:10.1186/s40645-016-0084-7

Review
Open Access
Published: 04 July 2016

Magnetohydrodynamics modeling of coronal magnetic field and solar eruptions based on the photospheric magnetic field

Satoshi Inoue^1,2

Progress in Earth and Planetary Science volume 3, Article number: 19 (2016) Cite this article

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Abstract

In this paper, we summarize current progress on using the observed magnetic fields for magnetohydrodynamics (MHD) modeling of the coronal magnetic field and of solar eruptions, including solar flares and coronal mass ejections (CMEs). Unfortunately, even with the existing state-of-the-art solar physics satellites, only the photospheric magnetic field can be measured. We first review the 3D extrapolation of the coronal magnetic fields from measurements of the photospheric field. Specifically, we focus on the nonlinear force-free field (NLFFF) approximation extrapolated from the three components of the photospheric magnetic field. On the other hand, because in the force-free approximation the NLFFF is reconstructed for equilibrium states, the onset and dynamics of solar flares and CMEs cannot be obtained from these calculations. Recently, MHD simulations using the NLFFF as an initial condition have been proposed for understanding these dynamics in a more realistic scenario. These results have begun to reveal complex dynamics, some of which have not been inferred from previous simulations of hypothetical situations, and they have also successfully reproduced some observed phenomena. Although MHD simulations play a vital role in explaining a number of observed phenomena, there still remains much to be understood. Herein, we review the results obtained by state-of-the-art MHD modeling combined with the NLFFF.

Review

Introduction

Solar flares are explosive phenomena observed in the atmosphere of the Sun (the solar corona). These events are observed as sudden bursts of electromagnetic radiation, such as extreme ultraviolet radiation (EUV), X-rays, and even white light; some examples are shown in Fig. 1 a–c. The scale is classified as soft X-rays, using the 1–8 Å band obtained by the GOES-5 satellite (one of the Geostationary Orbiting Environment Satellites), as shown in Fig. 1 d. The Sun is known to be a magnetized star. Figure 2 a shows the line-of-sight component of the magnetic field, and the positive and negative polarities cover the whole sun. Figure 2 b shows the three-dimensional (3D) magnetic field lines traced from the positive to the negative polarities; these have been extrapolated under the assumption of the potential field approximation (this will be discussed below). Solar flares often occur above the sunspots corresponding to a cross section of strong magnetic flux. In addition, because the solar corona satisfies the low- β plasma condition (β= 0.01–0.1) (Gary 2001) in which the magnetic energy dominates that of the coronal plasma, solar flares are widely considered to be a manifestation of the conversion of the magnetic energy of the solar corona into kinetic and thermal energy, culminating in the release of high-energy particles and electromagnetic radiation. Figure 2 c is an enlarged view of the region that is marked by an arrow in Fig. 2 b; here, the field lines are responsible for the current density accumulation, which initiates the flare. These field lines are extrapolated using the nonlinear force-free field (NLFFF) approximation; this is one of the main topics of this paper.

Furthermore, this causes a huge amount of coronal gas (a typical mass is 10¹⁵ g) with a velocity of 100–2000 kms ⁻¹ to be released into interplanetary space; this is called a coronal mass ejection (CME; e.g., Forbes (2000)). The CMEs are sometimes associated with solar flares; however, the detailed understanding of the relationship between these two phenomena remains elusive (Chen 2011; Schmieder et al. 2015). It is important to understand these phenomena in order to better understand the nonlinear plasma dynamics of the processes involving the magnetic energy or helicity of the solar coronal plasma; this includes storage-and-release processes as well as the forecasting space weather (Tóth et al. 2005; Liu et al. 2008; Kataoka et al. 2014). Investigations of solar flares and CMEs are thus important in terms of both the elemental plasma physics and the applied science.

Since the discovery of the solar flares by Carrington (1859), many studies have been performed (including observational, theoretical, and numerical studies) for clarifying their dynamics (Benz 2008; Priest and Forbes 2002; Shibata and Magara 2011; Wang and Liu 2015). Many new insights on solar flares and related phenomena have been obtained by analyzing the data collected by satellites. For instance, the Yohkoh satellite obtained much data on dynamical features of the sun, some of which had not been predicted; this can be seen in Fig. 3 a; this image, taken by a soft X-ray telescope, shows several important aspects that have helped our understanding of solar flares. For example, Tsuneta et al. (1992) discovered the cusp-shaped structure during the solar flare seen in the lower right panel in Fig. 3 a. A detailed analysis (Tsuneta 1996) produced evidence of the reconnection, and this lent support to a theoretical flare model based on reconnection; this model is named for its developers, Carmichael, Surrock, Hirayama, Kopp, and Pneumann (CSHKP) and explains the observations at multiple wavelengths (Carmichael 1964; Hirayama 1974; Kopp and Pneuman 1976; Sturrock 1966). Masuda et al. (1994) confirmed the CSHKP model of the solar flare by analyzing the hard X-ray signals obtained during a solar flare. In addition, Sterling and Hudson (1997) found a characteristic pattern of X-rays that are released prior to a flare; this is shown in the upper right panel of Fig. 3 a. This pattern is a sigmoid (an S- or inverse S-shaped structure) that changes into a cusp-shaped loop structure after the flare occurs. Su et al. (2007) and McKenzie and Canfield (2008) demonstrated the fine structure and topology of the field lines that were later observed by an X-ray telescope (Golub et al. 2007) on board the Hinode satellite (Kosugi et al. 2007). In addition, Yokoyama et al. (2001) found evidence of reconnection inflow in extreme ultraviolet observations of the Solar and Heliospheric Observatory (SOHO). The images of the coronal loop shown in Fig. 3 b are reminiscent of reconnection. Because these observations were based on imaging of electromagnetic waves, the data were mapped onto a 2D plane. Thus, obtaining a 3D reconstruction of these events is extremely difficult.

Based on this observational evidence, there have been several attempts to construct the 3D magnetic structure (e.g., Shibata (1999)). Figure 3 c is an image of a 3D magnetic structure inferred from observations during the onset of the solar eruption depicted in Shiota et al. (2005); the reconnection model can be used to explain various observed phenomena, e.g., the two H- α flare ribbons, and giant arcades. In addition, various models have been proposed that predict the onset of solar flares and CMEs. For instance, Forbes and Priest (1995) proposed the catastrophic model shown in Fig. 3 d; this shows that the flux tube in the solar corona does not remain at equilibrium when the boundary conditions are changed, and this results in a sudden eruption. The tether-cutting model, proposed by Moore et al. (2001), is shown in Fig. 3 e. They assumed that two sheared field lines existed along the polarity inversion line (PIL) prior to the onset of the flare; this is shown in the upper left panel of Fig. 3 e. Note that this has a somewhat sigmoidal structure. If there is reconnection between the sheared field lines, then long twisted lines are formed, and an eruption may occur. The final state shown in the right bottom panel of Fig. 3 e is very similar to that shown in Fig. 3 c.

The dramatic increase in computer power allows us to perform 3D magnetohydrodynamics (MHD) simulations and to estimate the 3D dynamics of magnetic fields during solar flares. Several studies have modeled sunspots to be asymmetric or as simple dipole fields and have analytically obtained the 3D coronal magnetic fields by fitting appropriate boundary conditions (e.g., Amari et al. (2000) and Amari et al. (2003a)). Figure 4 a shows the results from Amari et al. (2003b); this shows the formation of a flux tube, which is initiated by the initial potential field, through twisted and converged motion on the photosphere. The twisted motion imposed on a dipole sunspot causes the accumulation of sheared field lines, and the motion converging toward the PIL creates a flux tube composed of highly twisted field lines due to the flux cancellation. Aulanier et al. (2012) and Janvier et al. (2013) constructed similar MHD models, and these generated a 3D view that extended the well-established 2D CSHKP model. This view produced a 3D feature that was not seen in the 2D model; their simulations produced strong-to-weak sheared post-flare loops, which are consistent with observations (Asai et al. 2003). On the other hand, Kusano et al. (2012) successfully reproduced an eruption in a different way, as shown in Fig. 4 b. They created a linear force-free field that had shearing field lines as the initial condition; a small dipole emerging flux was imposed at a local area on the PIL. They found that only two types of emerging flux can produce a flux tube; this shows that the eruption is due to interactions with a pre-existing sheared magnetic field. Later, this scenario was confirmed in observations by Toriumi et al. (2013) and Bamba et al. (2013).

Other MHD models have been derived from an initialized flux tube. Solar filaments are often observed on the sun; these are composed of a denser plasma than that in the solar corona (Parenti 2014). It is widely agreed that the highly helical twisted lines in the filament sustain the dense plasma in the solar corona (Priest and Forbes 2002). Recent observations clearly show the helical structure of the magnetic field, i.e., the flux tube and the dynamics (e.g., Cheng et al. (2013); Nindos et al. (2015); Vemareddy and Zhang (2014)). In addition to this, the flux tube/filaments have often been observed to erupt away from the solar surface. Following these observations, extensive MHD modeling, focusing on the flux tube dynamics, has been performed. Inoue and Kusano (2006) investigated the dynamics of a flux tube that was initially embedded in the solar corona, as shown in Fig. 4 c. This extended the studies of Forbes (1990) and Forbes and Priest (1995) showing the dynamics in a 2D space. This study found that the flux tube eruption was caused by a kink instability in 3D space, rather than by a loss of equilibrium in 2D space, as discussed by Forbes (1990). Recently, a higher-resolution simulation was performed by Nishida et al. (2013), who reported complex reconnections and plasmoid motions associated with flux tube eruption. Chen and Shibata (2000) numerically confirmed that a flux tube eruption is triggered by a small emerging flux that is the result of the reconnection with magnetic fields lines surrounding the flux tube, and it can reduce the downward tension force acting on the flux tube. Török et al. (2009) extended this into 3D space. As shown in Fig. 4 d, Török and Kliem (2005) and Fan (2005) constructed more realistic MHD models by noting that the flux tube roots are tied to the solar surface (Titov and Démoulin 1999), rather than by assuming infinitely long flux tubes as in Inoue and Kusano (2006) and Nishida et al. (2013). Török and Kliem (2005) reported that the eruption depends on the decay rate of the external magnetic field, and later, this scenario was explained as torus instability (Kliem and Török 2006). To address this instability, detailed stability and equilibrium analyses of flux tubes in the solar corona were performed by Isenberg and Forbes (2007) and Démoulin and Aulanier (2010), and the dynamics were numerically confirmed by Török and Kliem (2007), Fan (2010), and Aulanier et al. (2010). Attempts are being made to meet the challenge of simulating a solar eruption through the emergence of highly twisted flux tube embedded in the convection zone (e.g., An and Magara (2013); Archontis et al. (2014); Leake et al. (2014)).

Several studies have shown the formation and dynamics of a large-scale CME in the range of a few solar radii. Antiochos et al. (1999) proposed a breakout model in which a moving magnetic field surrounding the core fields triggers the CME; those dynamics were later confirmed in a high-resolution simulation (e.g., Lynch et al. (2008) and Karpen et al. (2012)). Shiota et al. (2010) reported that an interaction between the core field (modeled as a spheromak) and the ambient field is important for determining whether an ejection will occur.

However, most of the studies presented above assumed hypothetical and ideal situations. Although these studies clarified many elementary physical processes related to the onset and dynamics of solar flares, they did not incorporate the data collected by solar satellites (in particular, they did not incorporate magnetic field data). One of the reasons for this is that only the photospheric magnetic field can be measured, and this implies that the coronal magnetic field cannot be observed directly. Nevertheless, several models have been proposed in which the photospheric magnetic field is treated as a boundary surface (.e.g., Török et al. (2011); van Driel-Gesztelyi et al. (2014); Zuccarello et al. (2012)). Challenging simulations considered a wide domain that extended from the Sun to the Earth; their major objectives included the initiation of a CME, its propagation in interplanetary space, and ultimately its interaction with the magnetosphere, which governs the dynamics of the ionosphere (Manchester et al. 2004; Tóth et al. 2005).

On the other hand, most of these models employed only the normal components of the magnetic field, neglecting the horizontal fields. Horizontal magnetic fields are very important for explaining the solar flares because these fields serve as a proxy for the extent to which the field lines are twisted and sheared, i.e., for determining the free magnetic energy at the solar surface. The MHD modeling of solar eruptions, which accounts for the three components of the photospheric magnetic field, has only recently been demonstrated, thanks to a state-of-art solar physics satellite. However, several problems remain open; these include the uniqueness of the numerical solution and the mathematical consistency of the MHD equations on a specified boundary (these questions will be discussed below).

In this paper, we present state-of-the-art MHD modeling, which accounts for the photospheric magnetic field, and we will focus on applying this to solar eruptions. In particular, we introduce the modeling of the coronal magnetic field and solar eruptions, based on the three components of the photospheric magnetic field. This area of research has been recently revived, beginning with a study by Jiang et al. (2013), and followed by Inoue et al. (2014a), Amari et al. (2014), and Inoue et al. (2015). The structure of this article is as follows. We first introduce a method for 3D reconstruction of the coronal magnetic field, based on the photospheric magnetic field; this includes a potential field that is easily reconstructed from one of the components of these fields and a nonlinear force-free field that is based on all of the components. Next, we describe recent MHD models that use a magnetic field that is reconstructed from the measured photospheric field. Finally, we draw some important conclusions.

Extrapolation of the coronal magnetic fields

Because we can obtain observations of the magnetic field components only for the photosphere, it is necessary to extrapolate to obtain information about the 3D coronal magnetic fields in 3D. The solar corona is considered to be in low- β plasma state, where β=P/2B ² is defined to be the ratio of the plasma gas pressure (P) to the magnetic pressure (B ²). From this, we have that the force-free state

$$ \boldsymbol{J} \times \boldsymbol{B} =0 $$

(1)

is a good approximation for describing the state of the coronal magnetic field, where B is the magnetic field satisfying the solenoidal condition,

$$ \mathbf{\nabla}\cdot \boldsymbol{B} =0, $$

(2)

and J is the current density,

$$ \boldsymbol{J}=\mathbf{\nabla}\times \boldsymbol{B}. $$

(3)

In this section, we introduce a method for extrapolating the solar coronal magnetic field given only the photospheric magnetic fields in the force-free approximation.

Potential field

The potential field is the simplest force-free field approximation:

$$ \mathbf{\nabla} \times \boldsymbol{B} = 0, $$

(4)

where the current density vanishes everywhere. In this formulation, the magnetic field can be replaced with the scalar function ψ, as follows:

$$ \boldsymbol{B} = -\mathbf{\nabla} \psi. $$

(5)

If we use the solenoidal condition of Eq. (2), then Eq. (5) can be rewritten as

$$ \nabla^{2}\psi = 0. $$

(6)

This corresponds to the Poisson equation, for which a unique solution is guaranteed for a boundary valueproblem. In this way, we can calculate the solar coronal magnetic field, given the normal component of the magnetic field (B _n) and its Neumann condition,

$$ B_{n}=\frac{\partial \psi}{\partial n}, $$

(7)

on each boundary. Although the photospheric magnetic field can be considered to be the bottom surface, conditions are required on the other boundaries in order to solve Eq. (6). Several such methods have been proposed, some of which are described below.

One approach is to use Green’s functions (Sakurai 1982; 1989). In this approach, the potential field is created by monopoles that are located at different points on the bottom boundary (x ^′,y ^′,0), at which the magnetic flux B _z d x ^′ d y ^′ exists. The scalar potential ψ is

$$ \psi =\frac{1}{2 \pi}\int B_{n}\left(x^{'},y^{'}\right)G\left(x,y,z,x^{'},y^{'}\right)dx^{'}dy^{'}, $$

(8)

where $G=1/\sqrt {|\boldsymbol {r}^{'}-\boldsymbol {r}|}$. The scalar function is determined automatically by the normal component of the observed magnetic field, whereas B=0 is assumed as r approaches ∞. This method can be applied to an isolated active region that is not influenced by the magnetic fields of other regions. On the other hand, if the magnetic field lines in the active region extend into another active region, the boundary conditions at the sides and top are no longer appropriate.

The Fourier expansion can be used for deriving the solution of Eqs. (5) and (6). The solution was presented by Priest (2014), as follows:

$$\begin{array}{@{}rcl@{}} B_{x} = -\sum_{\boldsymbol{k}} \frac{k_{x}}{|k|}B_{\boldsymbol{k}}e^{ik_{x}+{ik}_{y}-kz}, \\ B_{y} = -\sum_{\boldsymbol{k}} \frac{k_{y}}{|k|}B_{\boldsymbol{k}}e^{ik_{x}+{ik}_{y}-kz}, \\ B_{z} = B_{0}+\sum_{\boldsymbol{k}} B_{\boldsymbol{k}}e^{ik_{x}+{ik}_{y}-kz}, \end{array} $$

(9)

where the bottom boundary values are expanded into Fourier components k _x and k _y. This formulation implies that all of the components decay exponentially, implying B=0 at z=∞. However, the side boundaries automatically obey periodic boundary conditions, so this method is useful only for describing areas far from the side boundaries.

We can easily extend Eq. (6) in spherical coordinates (r, θ, ϕ) and thus obtain a solution for the whole sun, as shown in Fig. 2 b. This overcomes the problem mentioned above regarding the connectivity of the field lines. In spherical coordinates, the solution to Eq. (6) can be written using Legendre polynomials (Altschuler and Newkirk 1969), as follows:

$$ {}\psi = \sum_{n=1} \sum_{m=0} \left[\left(\frac{1}{r}\right)^{n+1}\left({g^{m}_{n}}\text{cos} \phi + {h_{n}^{m}}\text{sin} \phi \right) {P^{m}_{n}}\left(\text{cos} \theta\right)\right], $$

(10)

where ${P^{m}_{n}}(cos \theta)$ are Legendre polynomials, and ${g_{n}^{m}}$ and ${h_{n}^{m}}$ are coefficients obtained from spherical harmonics analysis. The boundary condition is based on the normal component of the photospheric magnetic field, and the Neumann condition of ψ is the same as that in Eq. (7). Using the above calculations, the potential fields can be expressed as follows:

$$ \begin{aligned} {} B_{r} &\,=\, - \sum_{n=1}^{N} \sum_{m=0}^{n}\! \left\{\!(n\,+\,1)\!\left(\frac{1}{r}\right)^{n+2}\!\left({g_{n}^{m}}\text{cos} \phi \,+\, {h_{n}^{m}}\text{sin} \phi\right)\! {P^{m}_{n}}\!\left(cos \theta\right) \right\},\\ {} B_{\theta} &\,=\, \sum_{n=1}^{N} \sum_{m=0}^{n} \left\{\left(\frac{1}{r}\right)^{n+2}\left({g_{n}^{m}}\text{cos} \phi + {h_{n}^{m}}\text{sin} \phi\right) \frac{d {P^{m}_{n}}\left(\text{cos} \theta\right)}{d \theta}\right\}, \end{aligned} $$

(11)

$$ \begin{aligned} B_{\phi} \,=\, - \sum_{n=1}^{N} \sum_{m=0}^{n} \left\{m\left(\frac{1}{r}\right)^{n+2}\left({g_{n}^{m}}\text{sin} \phi - {h_{n}^{m}}\text{cos} \phi\right) \frac{{P^{m}_{n}}\left(\text{cos} \theta\right)}{\text{sin} \theta}\right\}. \end{aligned} $$

(12)

As an example, one result is shown in Fig. 2 b, which can be used to depict the field lines covering the sun.

One advantage of the potential field extrapolation method is that the solution is relatively easily obtained; there are several techniques for doing this. On the other hand, the potential field is a minimum energy state that does not store the free magnetic energy released in the solar flares. This implies that the observed field lines in the area close to the PIL cannot be captured by the potential field. To convert the potential field into the dynamic phase of the solar flares, it is necessary to obtain the Poynting flux through the photosphere in order to obtain the free energy (Feynman and Martin 1995; van Ballegooijen and PMartens 1989).

Linear force-free field

The force-free Eq. (1) can be rewritten as

$$ \mathbf{\nabla} \times \boldsymbol{B} = \alpha \boldsymbol{B}, $$

(13)

where α is a coefficient. After taking the divergence of this equation, the left-hand side vanishes, and thus, we have

$$ (\boldsymbol{B} \cdot \mathbf{\nabla}) \alpha = 0, $$

(14)

which implies that the coefficient α is constant along all field lines. If the coefficient α is constant everywhere (not only along the field lines), Eq. (13) becomes a linear Equation that can be reduced to the Helmholtz equation,

$$ \nabla^{2} \boldsymbol{B} + \alpha \boldsymbol{B}=0, $$

(15)

by taking the curl of Eq. (13). We call this solution the linear force-free field (LFFF), and it is also specified with an appropriate boundary condition.

For example, (Chiu and Hilton 1977) found the analytical general solution by using Green’s functions:

$$ \begin{aligned} B_{i} = \frac{1}{2\pi} \int^{\infty}_{-\infty}dx'dy' \left[ \overline{G_{i}}(\boldsymbol{x},\boldsymbol{x}')B_{z}(x',y',0) + \tilde{G_{i}}(\boldsymbol{x},\boldsymbol{x}')C(x',y') \right], \end{aligned} $$

(16)

where C(x ^′,y ^′) is any finite integrable function (see Chiu and Hilton (1977)). $\tilde {G_{i}}(\boldsymbol {x},\boldsymbol {x}')$ is defined as

$$\begin{array}{@{}rcl@{}} &&\overline{G_{x}} =\frac{x-x'}{R} \frac{\partial \overline{\Gamma}}{\partial z} + \alpha \overline{\Gamma} \frac{y-y'}{R}, \\ &&\overline{G_{y}} =\frac{y-y'}{R} \frac{\partial \overline{\Gamma}}{\partial z} - \alpha \overline{\Gamma} \frac{x-x'}{R}, \\ &&\overline{G_{z}} = - \frac{\overline{\Gamma}}{\partial R} - \frac{\overline{\Gamma}}{R}, \end{array} $$

where R=(x−x ^′)²+(y−y ^′)², $\overline {\Gamma }$ is

$$\begin{array}{@{}rcl@{}} \overline{\Gamma} = \frac{z}{Rr}\text{sin}(\alpha r) - \frac{1}{R}\text{sin}(\alpha z), \end{array} $$

and r=(x−x ^′)²+(y−y ^′)²+z ². Using these equations, if we are given B _z and the force-free α at the photosphere, then the LFFF is automatically determined.

Unlike the potential field, the LFFF can yield the free magnetic energy. In general, however, the observed force-free α measured in the photosphere varies in space. In particular, in solar active regions, the coefficient α attains high values close to the PIL and small values far from the PIL. This implies that the LFFF is inappropriate for modeling solar active regions. Therefore, we need to obtain the NLFFF extrapolation by using the observed force-free α, i.e., we need to obtain not only the normal component of the magnetic field but also the horizontal components at the photosphere in order to reproduce the magnetic field of a solar active region.

Nonlinear force-free field

To demonstrate suitable magnetic fields in the solar active region, we consider solving the force-free Eq. (1) directly. However, because this equation contains nonlinearities that cannot be solved analytically, numerical techniques are necessary (i.e., Schrijver et al. (2006) or Metcalf et al. (2008)). Since important information can be obtained from observed photospheric magnetic fields, this becomes a boundary value problem. Below, we briefly describe several numerical methods that have been developed.

Vertical integration method. The algorithm of the vertical integration method is quite simple. The magnetic fields are integrated upward in the z direction, as originally proposed by Nakagawa (1974) and further extended by Wu et al. (1990). Under the force-free assumption, the current densities of the horizontal components along the solar surface can be calculated as follows:

$$\begin{array}{@{}rcl@{}} J_{x0} = \alpha_{0} B_{x0}, \\ J_{y0} = \alpha_{0} B_{y0}, \end{array} $$

(17)

where B _x0 and B _y0 are the horizontal components of the photospheric magnetic field, J _x0 and J _y0 are the horizontal components of the current density, and α ₀ is the force-free alpha obtained from J _z0/B _z0. Using Ampere’s law, Eq. (3), and the solenoidal condition, Eq. (2), the following equations are obtained for the z-derivatives of the magnetic field:

$$\begin{array}{@{}rcl@{}} && \frac{\partial B_{x}}{\partial z} = J_{y0} + \frac{\partial B_{z0}}{\partial x}, \\ && \frac{\partial B_{y}}{\partial z} =\frac{\partial B_{z0}}{\partial y} - J_{x0}, \\ && \frac{\partial B_{z}}{\partial z} = -\frac{\partial B_{x0}}{\partial x} - \frac{\partial B_{y0}}{\partial y}. \end{array} $$

(18)

The integration, in which the information about the photospheric magnetic field is extended upward, is repeated, and the coronal magnetic field can be calculated in 3D. However the above algorithm is mathematically ill-posed, i.e., the calculation is not robust, as has been reported in several papers (e.g., Wiegelmann and Sakurai (2012)). For instance, once the nonphysical phenomena due to numerical errors appear during the integration, the magnetic field increases exponentially. One reason for this is that no restrictions are imposed on the top and side boundaries.

The Green’s function method. A similar mathematical approach that uses the Green’s function was developed by Yan (1995) and Yan and Sakurai (2000) but the magnetic field is assumed as follows: $\boldsymbol {B}=O\left (\frac {1}{r^{2}}\right)$, i.e., B = 0 as r=>∞. They found the NLFFF solution based on Green’s second identity, as follows:

$$ c_{i}\boldsymbol{B}_{i} = \int_{S} \left(\boldsymbol{Y}\frac{d\boldsymbol{B}}{dn} - \frac{d\boldsymbol{Y}}{dn}\boldsymbol{B}_{0}\right)dS, $$

(19)

where c _i=1 and c _i=1/2 correspond to points in the volume and at the boundary, respectively, B ₀ is the measured photospheric magnetic field, and Y is a reference function,

$$ \boldsymbol{Y}(r) = \frac{cos(\lambda_{i} \boldsymbol{r})}{4 \pi |\boldsymbol{r}-\boldsymbol{r}'|}, $$

(20)

where r ^′ is a fixed point and λ(r ^′) is a parameter that depends on r ^′. The reference function satisfies the Helmholtz equation,

$$ \nabla^{2} \boldsymbol{Y} + \lambda^{2} \boldsymbol{Y} = \delta_{i}, $$

(21)

where δ _i is the Dirac delta function. The parameter λ _i can be obtained by solving

$$ \int_{V} Y_{i}({\lambda_{i}^{2}} B_{i} - \alpha^{2} B_{i} - (\nabla \alpha \times \boldsymbol{B}_{i}))dV =0. $$

(22)

Although it has been pointed out that this technique is slow (Wiegelmann and Sakurai 2012), recently, the calculation speed has been dramatically accelerated by using a GPU (Wang et al. 2013).

Grad-Rubin method. Sakurai (1981) was the first to use the Grad-Rubin method for calculating the magnetic field in solar active regions, and this method was later extended, e.g., Amari et al. (2006). This technique follows directly from the force-free field property. First, the potential field is calculated based only on the normal components of the magnetic field. The force-free α can be measured at the bottom surface as α=J _z/B _z, and it can be distributed in 3D according to the following equation:

$$ \boldsymbol{B}^{k} \cdot \nabla{\alpha}^{k} = 0, $$

(23)

where k is the iteration number and B ⁰ corresponds to the potential field. The magnetic field is updated according to

$$ \mathbf{\nabla} \times \boldsymbol{B}^{k+1} = \alpha^{k} \boldsymbol{B}^{k}, $$

(24)

and

$$ \mathbf{\nabla} \cdot \boldsymbol{B}^{k+1} = 0. $$

(25)

Since the vector potential A ^k satisfying ∇×A ^k=B ^k can be written as

$$ {}\boldsymbol{A}^{k+1} = \int \frac{\boldsymbol{J}^{k}}{\sqrt{(x-x')^{2}+(y-y')^{2}+(z-z')^{2}}}dx'dy'dz', $$

(26)

the updated B automatically satisfies the solenoidal condition, and it is then substituted back into Eq. (23). This process is repeated until the magnetic field reaches a steady state. Although the force-free α can be determined at positive or negative polarity and will satisfy Eq. (23), the single-polarity information is neglected. Nevertheless, Régnier et al. (2002) and Canou and Amari (2010) were able to reconstruct magnetic fields that agree with the observations.

Recently, the Grad-Rubin method has been improved by Amari et al. (2010); Wheatland and Régnier (2009), and (Wheatland and Leka 2011), who have obtained the unique solution by using two different solutions derived from different polarities, i.e., by changing the distribution of the force-free α at the bottom surface.

MHD relaxation method. In the MHD relaxation methods, the MHD equations are solved directly (in particular, this is the zero-beta MHD approximation (Mikić et al. 1988)); they solved

$$ \frac{\partial \boldsymbol{v}}{\partial t} = - (\boldsymbol{v}\cdot\mathbf{\nabla})\boldsymbol{v} + \boldsymbol{J}\times\boldsymbol{B} + \nu\mathbf{\nabla}^{2}\boldsymbol{v}, $$

(27)

$$ \frac{\partial \boldsymbol{B}}{\partial t} = \mathbf{\nabla}\times(\boldsymbol{v}\times\boldsymbol{B} - \eta\boldsymbol{J}), $$

(28)

and

$$ \boldsymbol{J} = \mathbf{\nabla} \times \boldsymbol{B} $$

(29)

to find the force-free solution while keeping the photospheric magnetic field as the boundary condition. Here, v is the plasma velocity, and ν and η are the viscosity and resistivity, respectively. The zero-beta MHD is an extreme approximation of the low-beta solution. However, since a force-free state can be assumed in the zero-beta approximation, this method is valid. Several studies (Mikić and McClymont 1994; McClymont and Mikic 1994; Jiang and Feng 2012; Inoue et al. 2014b) have employed the potential field as the initial condition; consequently, the magnetic twist on the bottom surface is obtained by replacing the tangential components of the photospheric magnetic field above which the magnetic fields relaxes toward the force-free state through the MHD relaxation process. This process is called the stress-and-relaxation method (Roumeliotis 1996). In a simpler treatment, known as the magnetofrictional method, the equation of motion (27) is replaced with

$$ \boldsymbol{v} = \mu\, \boldsymbol{J} \times \boldsymbol{B}, $$

(30)

where μ is a coefficient. This technique can also be used to find the force-free solution (Valori et al. 2005), and it has been applied to the photospheric magnetic field.

Note that if the three components of the photospheric magnetic field are fully satisfied at the solar surface and if the plasma velocity is zero there, these conditions are not consistent with the induction equation, which requires information about the differential value in the normal direction. Consequently, an error appears in ∇·B. Therefore, the errors arising during the relaxation process should be eliminated, and several methods have been developed for eliminating them (Tóth 2000; Miyoshi and Kusano 2011). Often, the projection method is used, and this removes the errors derived from the potential component. We decompose the numerically obtained magnetic field B _N into B _p (the potential component) and B _np (the non-potential component), as follows:

$$ \boldsymbol{B}_{N} = \boldsymbol{B}_{p} + \boldsymbol{B}_{np}. $$

(31)

In general, a vector field B can be described as

$$ \boldsymbol{B} = \mathbf{\nabla}\psi_{p} + \mathbf{\nabla} \times \boldsymbol{A}_{np}, $$

(32)

where ψ _p and A _np are the scalar and vector potentials, respectively. Taking into account Eq. (5), ∇ ψ _p and ∇×A _np correspond, respectively, to the potential and non-potential components of the magnetic field. Taking the divergence of Eq. (32), the equality ∇·∇×A _np=∇·B _np=0 is automatically satisfied. However, it is not guaranteed that ∇·∇ ψ _p=∇·B _p= 0. If B _p contains a numerical error, we further decompose it into $\boldsymbol {B}_{p^{\prime }}$, which satisfies the solenoidal condition, and B _error, the error, as follows:

$$ \boldsymbol{B}_{p} = \boldsymbol{B}_{p'} + \boldsymbol{B}_{\text{error}}, $$

(33)

where, in general, B _error does not meet the solenoidal condition. However, taking the divergence of Eq. (33), the equation can be reduced to the Poisson equation,

$$ \mathbf{\nabla}\cdot\boldsymbol{B}_{\text{error}} = \mathbf{\nabla}\cdot \boldsymbol{B}_{N} = \nabla^{2} \psi_{p}. $$

(34)

Consequently, this equation can be solved, and the magnetic field satisfying the solenoidal condition B ^′ can be updated as follows:

$$ \boldsymbol{B}' = \boldsymbol{B}_{N} - \mathbf{\nabla}\psi_{p}. $$

(35)

This technique has been widely used for eliminating errors (Tanaka 1995; Tóth 2000); however, solving the Poisson equation is computationally demanding. Therefore, numerical techniques for improving the calculation speed, e.g., a multigrid technique, are required (Inoue et al. 2014b).

Another technique was proposed by Dedner et al. (2002), who introduced a modified induction equation,

$$ \frac{\partial \boldsymbol{B}}{\partial t} = \mathbf{\nabla}\times(\boldsymbol{v}\times\boldsymbol{B} - \eta\boldsymbol{J}) - \mathbf{\nabla}\phi, $$

(36)

and a convenient equation for eliminating the errors derived from ∇·B,

$$ \frac{\partial \phi}{\partial t} + {c^{2}_{h}}\mathbf{\nabla}\cdot\boldsymbol{B} = -\frac{{c^{2}_{h}}}{{c^{2}_{p}}}\phi, $$

(37)

together with the equation of motion (27) and Ampere’s law (29). Using Eq. (36), Eq. (37) can be changed to

$$ \frac{\partial^{2} (\mathbf{\nabla}\cdot\boldsymbol{B})}{\partial t^{2}} + \frac{{c_{h}^{2}}}{{c_{p}^{2}}}\frac{\partial (\mathbf{\nabla}\cdot\boldsymbol{B})}{\partial t} = {c_{h}^{2}}\mathbf{\nabla^{2}}(\mathbf{\nabla}\cdot\boldsymbol{B}), $$

(38)

where c _h and c _p correspond to the advection and diffusion coefficients; this plays a role in propagating and diffusing the numerical errors of ∇·B. The main advantage of this method is that it can be implemented very easily without significantly changing the numerical code. Another advantage is that this method is less computationally demanding than the projection method. These advantages were demonstrated by Inoue et al. (2014b).

The vector potential is specified to maintain the solenoidal condition. Using the vector potential, the induction equation can be written as

$$ \frac{\partial \boldsymbol{A}}{\partial t} = -\boldsymbol{E} - \nabla{\Phi}, $$

(39)

where E=η J−v×B and Φ is the gage. Several papers have used the NLFFF extrapolation (e.g., van Ballegooijen et al. (2000) and Cheung and DeRosa (2012)). In this case, the solution is sought under the proper boundary conditions and gage. Simply, B _z and J _z are fixed at the boundary (i.e., A _x and A _y are fixed), then A _z is obtained from ∇² A=J under the Coulomb gage ∇·A=0. A solution obtained by this method will completely satisfy the solenoidal condition. On the other hand, there is no guarantee that the horizontal components at the bottom surface, which are obtained by iteration, will match observed values.

The constrained transport (CT) method (Brackbill and Barnes 1980; Evans and Hawley 1988) uses a numerical differential approach to maintaining the solenoidal condition. When the magnetic field B and electric field E are defined at the face center and edge centers of each numerical cell, i.e.,

$$\begin{array}{@{}rcl@{}} && \frac{d}{dt}B_{xi+1/2,j} = -\frac{E_{zi+1/2,j+1/2} - E_{zi+1/2,j- 1/2}}{\Delta y}, \\ && \frac{d}{dt}B_{yi,j+1/2} = \frac{E_{zi+1/2,j+1/2} - E_{zi- 1/2,j+1/2}}{\Delta x}, \end{array} $$

(40)

where symmetry is assumed in the z direction, then the solenoidal condition is automatically satisfied:

$$ \frac{d}{dt}\left(\frac{B_{xi+1/2,j} - B_{xi-1/2,j}}{\Delta x} + \frac{B_{yi,j+1/2} - B_{yi,j-1/2}}{\Delta y}\right) = 0. $$

(41)

However, the solenoidal condition requires consistent interaction with the boundary condition, and thus, it might be difficult to use it with the NLFFF calculations, which require the three components of the photospheric magnetic field.

Optimization method. Wheatland et al. (2000) proposed an optimization method that was later improved by Wiegelmann (2004). This method iteratively minimizes a function L related to J×B and ∇·B. First, we define a function L as

$$ L=\int \left(\frac{1}{B^{2}}\left|\left(\mathbf{\nabla}\times\boldsymbol{B}\right) \times \boldsymbol{B}\right|^{2} +\left|\mathbf{\nabla} \cdot \boldsymbol{B}\right|^{2}\right)dV; $$

(42)

it is the sum of the Lorentz force and the solenoidal condition, and its value is prescribed to be zero in order to satisfy the force-free condition. The time derivative is expressed as

$$ \frac{1}{2} \frac{dL}{d t} = -\int \frac{\partial \boldsymbol{B}}{\partial t}\cdot \boldsymbol{F}dV -\int \frac{\partial \boldsymbol{B}}{\partial t}\cdot \boldsymbol{G}dS, $$

(43)

where F and G are high-order differential equations in terms of B. If the function F satisfies

$$ \frac{\partial \boldsymbol{B}}{\partial t} = \mu \boldsymbol{F}, $$

(44)

and if the magnetic fields on the surface vanish at infinity, then the L monotonically decreases. The problem is then reduced to iteratively finding the steady state the time-dependent magnetic field B that satisfies Eq. (44).

NLFFF extrapolation using the observed images. van Ballegooijen (2004) modeled a filament by inserting a twisted magnetic flux tube, whose axis was along the observed filament, into a potential field, with the magnetofriction (van Ballegooijen et al. 2000) driving the system toward the force-free state. In this case, although the horizontal fields were not used, the filament and the sigmoid structure were satisfactorily reproduced (Bobra et al. 2008; Su et al. 2009; Savcheva et al. 2012). Rather than using the methods accounting for the photospheric horizontal fields, modeling the filaments in the quiet region would be very useful because the values are very weak and the directions are random, so this might depend on the observations. In an attempt to obtain consistent magnetic fields, several studies have considered the topology of the coronal loops obtained from images, in addition to accounting for the photospheric magnetic field (Aschwanden et al. 2014; Malanushenko et al. 2014).

Unfortunately, the NLFFF does not allow the full calculation of the coronal magnetic fields. First of all, because, in general, the photospheric magnetic field cannot satisfy the force-free state, there is a contradiction between the bottom and inner regions; consequently, the 3D-reconstructed field also deviates from the force-free state. Furthermore, although several methods have been developed for exploring the NLFFF, there are no guarantees that there is a unique solution that fits the photospheric magnetic field applied to a given boundary condition. In the NLFFF approach, there are several open problems related to the free magnetic energy or the topologies of the magnetic fields (Schrijver et al. 2008; De Rosa et al. 2009). Thus, there is a need for confirmation of the reliability of this approach.

NLFFF extrapolation applied to a reference field (Low and Lou 1990)

The above methods for the NLFFF reconstruction have been applied to the photospheric magnetic field observed in the solar active region. Most of these methods required knowledge of the reference magnetic field in order to determine to what extent the reconstructed field approaches the force-free state. One of the widely known solutions is a semi-analytical force-free field that was presented by (Low and Lou 1990). These authors found a force-free solution in spherical coordinates, where symmetry was assumed in the ϕ direction:

$$ \boldsymbol{B} = \frac{1}{r \text{sin} \theta}\left(\frac{1}{r} \frac{\partial A}{\partial \theta} \boldsymbol{r}, -\frac{\partial A}{\partial r} \mathbf{\theta}, Q \mathbf{\phi}\right), $$

(45)

where A and Q are functions of r and θ. The force-free Eq. (1) can be rewritten as

$$ \frac{\partial^{2} A}{\partial r^{2}} + \frac{1-\mu^{2}}{r^{2}} \frac{\partial^{2} A}{\partial \mu^{2}} +Q\frac{dQ}{dA} = 0, $$

(46)

where μ=cos(θ) and α=d Q/d A. It can be further rewritten as

$$ \left(1-\mu^{2}\right)\frac{\partial^{2} P}{\partial \mu^{2}} +n(n+1)P + a^{2}\frac{1+n}{n}P^{1+2/n}=0, $$

(47)

using a separable solution

$$ A(r, \theta)=\frac{P(\mu)}{r^{n}}, $$

(48)

and as

$$ Q(A)=aA^{1+2/n}. $$

(49)

These formulas are obtained under the assumption of a vanishing magnetic field as r→0, i.e., for positive n. Although we can write down the 1D differential equation with respect to P(μ), shown as Eq. (47), it cannot be solved analytically due to its nonlinearity. The solution of this equation, therefore, is obtained numerically. The boundary condition is that P = 0 at μ = −1 and 1, which was originally set by Low and Lou (1990), and the solution is called the Low and Lou solution. The boundary conditions are that B _θ and B _ϕ vanish along the axis, and the differential equation can be solved as a boundary value problem. One of the solutions is shown in Fig. 5 a; here, the solution was transformed to Cartesian coordinates, and n = 1 and a ² = 0.425 are assumed (see Low and Lou (1990) for details). The accuracy of the NLFFF was checked using this solution as the reference magnetic field.

Schrijver et al. (2006) estimated the accuracy of the NLFFF as reconstructed by various different methods; this included a semi-analytical force-free solution introduced by Low and Lou (1990). Their results suggest that the reconstruction accuracy is strongly method dependent, i.e., several methods satisfactorily captured the Low and Lou solution, although other methods failed. On the other hand, during the past decade, many efforts have been made to improve the numerical code for the NLFFF reconstruction (Amari et al. 2006; Valori et al. 2007; He and Wang 2008; Wheatland and Leka 2011; Jiang and Feng 2012; Inoue et al. 2014b).

Below, we review the results based on a recent extrapolation method that was proposed by Inoue et al. (2014b) and is based on the MHD relaxation method. The potential field was reconstructed, based only on the normal component of the boundary magnetic field. This result is shown in Fig. 5 b and differs significantly from the Low and Lou solution. Next, the reconstructed horizontal fields at the bottom surface were replaced by those of the Low and Lou solution, following which the magnetic fields in the domain were iteratively relaxed according to the equation of motion (27), the induction Eq. (36), Amperes law (29), and Eq. (37), which was used to correct the errors in ∇·B.

During the iterations, at all boundaries, the vector B was fixed to be equal that in the Low and Lou solution, the velocity was set to zero, and the Neumann condition was imposed on ϕ, i.e., ∂ ϕ/∂ n=0, where n is the direction perpendicular to the boundaries. In order to avoid a large discontinuity between the bottom and the inner domain, the velocity field was adjusted as follows. We defined v ^∗=|v|/|v _A|, and if v ^∗ became larger than v _max, the velocity was modified as follows:

$$ \boldsymbol{v} \Rightarrow \frac{v_{\text{max}}}{v^{*}} \boldsymbol{v}, $$

(50)

where, v _max= 1.0. The resistivity was given as follows:

$$ \eta = \eta_{0} + \eta_{1} \frac{|\boldsymbol{J}\times\boldsymbol{B}||\boldsymbol{v}|}{\mathbf{|B|}}, $$

(51)

where η ₀=3.75×10⁻⁵ and η ₁=1.0×10⁻³ (both are non-dimensional). The second term was introduced to accelerate the relaxation to the force free field, particularly in a weak-field region. In this study, ${c_{h}^{2}}$ and ${c_{p}^{2}}$ were set to 5.0 and 0.1, respectively; these values were selected by trial and error and depend on the boundary conditions, but it is best if the value of c _h is first set to account for the CFL condition. The viscosity was assumed as ν= 1.0×10³; the viscosity also plays an important role in smoothly connecting the boundaries and nearby inner region, which indirectly helps our MHD calculation. A more detailed explanation of this was presented by Inoue et al. (2014b).

Eventually, the final state obtained by using this method almost completely reproduced the Low and Lou solution, as shown in Fig. 5 c. Quantitative results were also presented. The force-free α was measured at both footpoints of all field lines, and this is shown in Fig. 5 d. The force-free α must be constant along the field lines, following Eq. (14), and from Fig. 5 d, it can be concluded that this relation is satisfied. In addition, the authors quantitatively evaluated the accuracy by following Schrijver et al. (2006), evaluating

$$\begin{array}{@{}rcl@{}} C_{\text{vec}} = \frac{\sum_{i} \boldsymbol{B}_{i}\cdot \boldsymbol{b}_{i}} {\sum_{i}|\boldsymbol{B}_{i}|^{2} \sum_{i}|\boldsymbol{b}_{i}|^{2}}, \\ \\ C_{\text{cs}} = \frac{1}{N} \sum_{i}\frac{\boldsymbol{B}_{i} \cdot \boldsymbol{b}_{i}} {|\boldsymbol{B}_{i}||\boldsymbol{b}_{i}|}, \\ \\ 1 - E_{\mathrm{M}} = \frac{1}{N}\sum_{i} \frac{|\boldsymbol{b}_{i} - \boldsymbol{B}_{i}|}{|\boldsymbol{B}_{i}|}, \\ \\ 1- E_{\mathrm{N}} = \frac{\sum_{i} |\boldsymbol{b}_{i} - \boldsymbol{B}_{i}|}{\sum_{i} |\boldsymbol{B}_{i}|}, \\ \\ \epsilon = \frac{\sum_{i} |\boldsymbol{b}_{i}|^{2}}{\sum_{i}|\boldsymbol{B}_{i}|^{2}}, \end{array} $$

(52)

where B and b are Low and Lou solution (reference solution) and the extrapolated solution, respectively, C _vec is the vector correlation, C _cs is the Cauchy-Schwarz inequality, E _M is the mean vector error, E _N is the normalized vector error, ε is the energy ratio, and N is the number of vectors in the field. Inoue et al. (2014b) obtained C _vec = 1.0, C _cs = 1.0, 1−E _N = 0.97, 1−E _M = 0.95, ε = 1.02, and these values were estimated over the entire region, which was divided into 64 × 64 × 64 grids (see Inoue et al. 2014b for details). They confirmed that the NLFFF can be reconstructed with high accuracy. Most of the recently developed methods allow for the recording of these values. Thus, it is possible to achieve force-free field extrapolation if the boundary condition completely satisfies the force-free condition.

NLFFF extrapolation applied to the solar active region

3D magnetic fields in the solar active region

In contrast to the NLFFF extrapolation using the Low and Lou solution, some problems arise when the bottom boundary is applied to the photospheric magnetic field. Schrijver et al. (2008) performed the NLFFF extrapolations by using the photospheric magnetic field observed by the Hinode satellite, corresponding to the period of 6 h before the X3.4-class flare that occurred in the solar active region 10930 on 13 December 2006. Different methods were applied for the NLFFF extrapolation. The authors pointed out a method-dependent accumulation of the free magnetic energy in the NLFFF. According to their calculations, a single NLFFF could yield sufficient free magnetic energy to produce an X-class flare. De Rosa et al. (2009) also performed the NLFFF extrapolation using different methods and for a different another active region (AR10953). They reported method-dependent configurations of the magnetic fields. From these results, it appeared that the NLFFF required further development.

Although the NLFFF remains problematic and does not enable the complete reproduction of the coronal magnetic field on the basis of photospheric data, several recent studies had roughly captured the field lines observed in EUV images, as well as processes involving stored-and-released magnetic energy, helicity, and flares (e.g., Canou and Amari (2010); Inoue et al. (2013); Vemareddy et al. (2013); Jiang and Feng (2013); Malanushenko et al. (2014); Aschwanden et al. (2014); Amari et al. (2014).

In what follows, we describe NLFFF results based on the MHD relaxation method developed by Inoue et al. (2014b); note that the above equations are identical to those used by Low and Lou. The potential field is first reconstructed as the initial condition, and the boundary conditions are almost identical to those in the previous calculation, except that the potential fields are now fixed at the side and top boundaries. The following procedure is used to determine the bottom boundary. During the iterative process, the transverse components(B _BC) at the bottom boundary are evaluated according to

$$ \boldsymbol{B}_{\text{BC}} = \zeta \boldsymbol{B}_{\text{obs}} + (1-\zeta) \boldsymbol{B}_{\text{pot}}, $$

(53)

where B _obs and B _pot are the transverse components of the observational and the potential field, respectively, and ζ is a coefficient ranging from 0 to 1. R is introduced as an indication parameter for the force-free state, defined as $R = \int |\boldsymbol {J}\times \boldsymbol {B}|^{2} dV$; when it drops below a critical value, denoted by R _min, then ζ increases as ζ=ζ+d ζ, where d ζ is given as a parameter. As ζ approaches unity, B _BC becomes consistent with the observational data. The vector fields include spurious forces that produce a sharp jump from the photosphere to the interior domain, and the above process can help to reduce their effects. In this study, R _min=5.0×10⁻³, d ζ=0.02, and v _max = 0.01. In the MHD equations, ${c_{h}^{2}}$ and ${c_{p}^{2}}$ are given as constant values, 0.04 and 0.1, respectively, and ν=1.0×10⁻³. The resistivity is included in Eq. (51), with η ₀=5.0×10⁻⁵ and η ₁=1.0×10⁻³. For further details, see Inoue et al. (2014b).

Figure 6 a shows the photospheric magnetic field 90 min before the M6.6-class flare that occurred on 13 February 2011. These data were obtained by a helioseismic and magnetic imager (HMI; Scherrer et al. (2012)) onboard the solar dynamics observatory (SDO) satellite (Pesnell et al. 2012). The upper and lower panels in Fig. 6 b show enlarged views of the central area in Fig. 6 a; the arrows derived from the horizontal magnetic fields in the potential field are shown in the upper panel, and those derived from the observed one are shown in the lower panel. Figure 6 c, d shows the magnetic field lines in the potential field and in the NLFFF approximation, respectively, superimposed on Fig. 6 a. In particular, the central part of the NLFFF, in which strong sheared field lines build up and the current density is enhanced significantly, differs from that of the potential field. Figure 6 e shows the 171 Å EUV images for the time period in Fig. 6 a; these were acquired by an atmospheric imaging assembly (AIA; Lemen et al. (2012)) on board SDO. The same field lines as in Fig. 6 d were superimposed on Fig. 6 e. Because it can be clearly seen that most of the field lines roughly correspond to these obtained from the EUV image, the NLFFF appears to satisfactory reproduce the field lines in the observed EUV image.

Stability analysis of the NLFFF

Magnetic field stability is an important issue in the studies of solar eruptions. Unfortunately, the photospheric magnetic field and the EUV or X-ray images do not allow for a quantitative stability analysis. On the other hand, the NLFFF might allow a quantitative analysis if we are given the 3D space information. One of the possible instabilities that can drive an eruption under the zero-beta assumption is a current driven, and one type current-driven instability is kink instability (Ji et al. 2003), which is determined by the magnetic twist of the poloidal field generated by the current in the flux tube (Kruskal and Kulsrud 1958). The magnetic twist (T _n) is related to the magnetic helicity; that is, the flux tube helicity is described by the following equation (Berger and Field 1984):

$$ H = (T_{n} + W_{r}){\Phi}^{2}, $$

(54)

where H is the magnetic helicity, Φ is the magnetic flux of the flux tube, and W _r is the magnetic writhe corresponding to the helical structure of the field line axis. The magnetic twist T _n indicates how much of the magnetic helicity is generated by the currents parallel to the flux tube (Berger and Prior 2006; Török et al. 2010); thus, T _n can be written as

$$ T_{n} = \int \frac{dT_{n}}{ds}dl = \int \frac{J_{||}}{4 \pi |\boldsymbol{B}|} dl, $$

(55)

where || indicates the component parallel to the field line, and the line integral $\int dl$ is taken along the magnetic field line of the flux tube. Using J _||=J·B/|B|, Eq. (55) can be further rewritten as

$$ T_{n} = \frac{1}{4\pi} \int \frac{\boldsymbol{J} \cdot \boldsymbol{B}}{ |\boldsymbol{B}|^{2}} dl. $$

(56)

If the magnetic fields meet the force-free condition, the magnetic twist can be written as

$$ T_{n} = \frac{1}{4\pi} \int \alpha dl =\frac{1}{4\pi} \alpha L, $$

(57)

where α is the force-free alpha, and L is the length of the field line (Inoue et al. 2011; Inoue et al. 2012a). Inoue et al. (2012b) and Inoue et al. (2013) performed a stability analyses on the NLFFFs of AR10930 and AR11158, both of which produced X-class flares. Below, we describe the results of one of these twist analyses (for AR11158). AR 11158 produced an X2.2-class flare at 01:50 UT on 15 February 2011; it exhibited a quadruple field, as shown in Fig. 7 a. The NLFFF based on the MHD relaxation method is shown in Fig. 7 b; strong twisted lines were formed in the central region. The twist T _n was calculated for all field lines according to Eq. (56), and the result is shown in Fig. 7 c. According to this result, most of the field lines were less than one turn, and none reached the critical twist of T _n=1.75, which is required for kink instability (Török et al. 2004). Therefore, it was concluded that the twisted lines prior to the X2.2-class flare produced by AR11158 would be stable with respect to kink instability. In another study, Jiang et al. (2014a) successfully reproduced a large twisted filament and checked its stability. It was reported that the twist did not reach the critical value required for kink instability. However, note that T _n in Eq. (56) is the local twist of an infinitesimal flux tube; this is not the same as the global twist of a macroscopic flux rope. In addition, there is no guarantee that the theoretical criteria are directly applicable to the NLFFF. In order to more strictly confirm the stability, a numerical stability analysis (Kusano and Nishikawa 1996; Inoue and Kusano 2006) and an MHD simulation would be useful.

Torus instability (Kliem and Török (2006); tested against observations by Liu (2008)) is also important for driving the flux tube into the upper corona, e.g., for triggering a CME (Isenberg and Forbes 2007; Aulanier et al. 2010; Démoulin and Aulanier 2010; Kliem et al. 2014). This instability is induced by a broken force balanced against the hoop force (Chen 1989), due to the flux tube current and the magnetic field suppressing the flux tube. The decay index,

$$ n(z) = - \frac{z}{|\boldsymbol{B}|}\frac{\partial |\boldsymbol{B}|}{\partial z}, $$

(58)

is a convenient parameter (Kliem and Török 2006) because the location where this instability takes place is specified by n=1.5, which was already confirmed by several numerical studies (Török and Kliem 2007; Aulanier et al. 2010; Fan 2010). This stability analysis can be applied to the NLFFF analysis. For example, Guo et al. (2010) reconstructed the NLFFF using the optimization method (Wiegelmann 2004). In contrast to Inoue et al. (2011), they found strongly twisted lines over the critical twist of the kink instability and its writhe motion during the flare while a confined eruption was observed. They pointed out that even though the twisted lines in the NLFFF were not stable with respect to the kink instability, they were stable with respect to the torus instability, i.e., the flux tube remains within the magnetic field satisfying n≤1.5 during the eruption. Regarding the AR11158 studied by (Inoue et al. 2014a), the decay index at the twisted lines formed in the NLFFF cannot reach the critical value of the torus instability, as shown in Fig. 7 d. Thus, the authors pointed out that the NLFFF was stable with respect to both torus instability and kink instability. On the other hand, for a different event, Jiang et al. (2014b) estimated the temporal evolution of the flux tube height obtained from the NLFFF in solar active region 11283, focusing on the X2.1-class flare that occurred at 22:20 UT on 6 September 2011. They found that the decay index at the flux rope axis reached the critical value for torus instability at the time at which the flare was generated, resulting in an instability-driven eruption.

As seen from these studies, the NLFFF enables us to quantitatively perform a stability analysis, which would be difficult to do based only on observations. Recently, highly accurate measurements of photospheric magnetic fields became available from two space satellites and ground observations; these have made the NLFFF a very useful tool for understanding the coronal magnetic field as well as for speculating on the onset and dynamics of solar flares.

MHD simulations of the solar eruptions based on the observational data

Necessity of MHD simulations combined with the NLFFF

Numerical modeling of the coronal magnetic field (potential field, LFFF, and NLFFF) successfully clarified many unknown issues with 3D magnetic fields that had not been revealed by observation. On the other hand, these models consider only the force-free equilibrium state, and they are thus not able to model dynamic states (in particular, energy-released processes) that occur during flare events, even though the buildup of energy occurs at a rate much slower than the Alfven time scale and thus can be handled by the NLFFF. MHD simulations can be used to reproduce such dynamic states.

The potential field does not strongly contribute to the magnetic field in the solar active region because there is no free energy available to induce dynamic behavior. For instance, Zuccarello et al. (2012) performed MHD simulations of solar eruptions, using the potential field as the initial condition. To obtain the solar eruption, the Poynting flux through the boundary was determined, and the authors provided the hypothetical shear and the convergence of the plasma on the solar surface. Consequently, the non-potential field was built up, and the sheared and converging motions helped to form the flux tube, resulting in an eruption (Figure 6 and Figure 8 in their paper). The hypothetical motions are important factors for building up the non-potential field, but these are much different from the observed ones. This means that there is a different process for the building up of energy, i.e., the magnetic field just prior to the onset of a flare deviates from the observed one. In contrast to this process, several studies inserted an analytical flux rope with a strong current and non-potentiality in a local area close to the PIL into the reconstructed potential field. Unfortunately, these flux tubes did not agree exactly with the observations, i.e., the boundary condition of the flux tube deviated greatly from the observations.

It might be possible to overcome the above problem by using MHD simulations with the NLFFF because the NLFFFs are constructed on the photospheric magnetic field, including the observed horizontal magnetic field on the solar surface. The motivations for using these simulations rather than the previous one are as follows: (i) It is likely that the artificial energy buildup process is not required by the existence of twisted motions because it already accounts for the observed twisting in the NLFFF. Although an additional process is required (discussed below) to create a new state that deviates from the NLFFF and produces eruptions, compared to the previous simulations, that process does not greatly deform the initial state. Therefore, MHD simulations can be performed under the photospheric magnetic field constraint. (ii) These simulations allow for the study of complex nonlinear dynamics, which could not be done previously. (iii) The results obtained from these simulations can be compared more exactly with observations, even indirect ones. Thus, these results contribute to confirming the reliability or to improving the MHD model. This field of study is emerging (Jiang et al. 2013), and only a few papers have yet been published. Below, we briefly discuss several of the pioneering studies.

MHD models of the solar eruptions, combined with the NLFFF

Overview of the recent studies. Jiang et al. (2013) were the first to perform the MHD simulation using the NLFFF to reproduce the X2.1-class flare in solar active region 11283. Their NLFFF, which was reconstructed by using the MHD relaxation method constructed in the modern MHD scheme (Feng et al. 2010), successfully captured the sigmoid structure of the magnetic field observed before the flare and demonstrated that the eruption was driven by the torus instability (Fig. 8 a). An important advantage of this study seems to be that the same algorithm was used in both the NLFFF and MHD simulations. Kliem et al. (2013) also studied this eruption by setting the NLFFF as the initial condition of their MHD simulation (Fig. 8 b). The NLFFF was reconstructed using the magnetic field observed on 8 April 2010, using the flux rope insertion and the magnetofrictional method. The NLFFF of this active region was thoroughly studied by Su et al. (2011). Kliem et al. (2013) found a critical value of the axial flux in the flux rope determined the stability. They reported that the criteria for the onset of a flare is that the axial flux be in the range of 5 × 10²⁰ to 6 × 10²⁰ Mx; in this case, the decay index is in the range of 1.3 to 1.8. For this eruption, the simulation results were in good agreement with some of the observations, such as those during the initial rising phase leading to the eruption. Amari et al. (2014) also successfully demonstrated a flux tube eruption in their MHD simulations, as shown in Fig. 8 c. The flux tube was reconstructed by using the Grad-Rubin type method (Amari and Aly 2010) combined with the photospheric magnetic field observed by the Hinode solar optical telescope (SOT; Tsuneta et al. (2008)) 6 h before the X3.4-class flare in AR10930 at 02:40 UT on 13 December 2006. The authors found that 6 h before the flare, the NLFFF was destabilized with flux cancellation, the gas motion in characteristic of a sunspot moat flow or photospheric turbulent diffusion, and this resulted in the eruption. On the other hand, 2 days before the flare, the NLFFF predicted no eruption for the same situation. The authors pointed out the importance of the formation of a significantly large flux tube and the moving out from equilibrium.

MHD modeling of the solar eruption on 15 February 2011. Inoue et al. (2014a) and Inoue et al. (2015) studied the magnetic field dynamics during the X2.2-class flare produced by solar active region 11158 on 15 February 2011 (Schrijver et al. 2011; Janvier et al. 2014; Yang et al. 2014), by using MHD simulations combined with the NLFFF. Figure 7 b shows the NLFFF structure approximately 2 h before the X2.2-class flare on 15 February 2011; note that strongly sheared magnetic fields lines are clearly visible at the PIL of the central sunspot. The stability analysis was discussed in a previous section. Based on these results, the NLFFF was quite stable, which implies that an additional process is required to drive the twisted lines. For instance, in a detailed data analysis, (Bamba et al. 2013) observed an increase in the small flux emerging at the PIL before the flare, and they suggested that this could destroy the stable magnetic field, as in the scenario described by Kusano et al. (2012).

The dynamics were investigated in the zero-beta MHD approximation, i.e., the density, pressure, and gravity were neglected. In such a situation, although the thermodynamics during the flare cannot be investigated, the magnetic field dynamics can be considered (Inoue et al. 2014a). This is the case because, during the flare, the magnetic energy converts into kinetic energy and thermal energy, which are the main factors for the energy store-and-release process in the solar corona. Therefore, in the early phase of a solar eruption that is not strongly compressible, zero-beta plasma is a good approximation, as demonstrated by Inoue and Kusano (2006). An advantage of this approximation is that it can neglect the sound waves, which often highly influence the rarefied CFL condition.

As discussed in the previous section, the NLFFF reconstructed 2 h before the X2.2-class flare shows a stable equilibrium state, and the dramatic dynamics that appear in observations are not evident. Therefore, some additional process is required to break the stable equilibrium. Here, Inoue et al. (2014a) and Inoue et al. (2015) introduced an anomalous resistivity imposed on the strong current region, and the MHD relaxation was performed by using the NLFFF as the initial condition where the velocity adjustment defined in Eq. (50) was removed. We would expect the anomalous resistivity to induce reconnection in the region of strong current density (Yokoyama and Shibata 2001) and to produce long twisted lines in the NLFFF. After an additional iteration, since there is no guarantee that this new state can remain in equilibrium, a newly created flux tube might escape from the solar surface, as was shown in Amari et al. (2014). The anomalous resistivity was

$$ \eta = \left\{ \begin{array}{ll} \eta_{0} & \quad \text{$J<j_{c}$}, \\ \eta_{0}+\eta_{2} \left(\frac{J-j_{c}}{j_{c}}\right)^{2} & \quad \text{$J>j_{c}$}, \end{array}\right. $$

(59)

where η ₀ is the background resistivity and j _c is the threshold current necessary to excite the second term in Eq. (59) (Yokoyama and Shibata 1994). In this study, η ₀=1.0×10⁻⁵, η ₂=1.0×10⁻⁴, and J _c = 30. It can initiate and enhance the reconnection in the strong current region when the current is greater than the critical value, J _c. This value depends on the normalized value of the coronal magnetic field defined in each study.

Figure 9 a shows two bundles of the twisted lines formed in the NLFFF; a strong current region was formed and sandwiched by these bundles. The side view is shown in Fig. 9 b. We expect that reconnection takes place between the two bundles of the twisted lines, and long, strongly twisted lines are formed, which might break the equilibrium. After additional iterations with the anomalous resistivity, the single long bundle of strongly twisted lines shown in Fig. 9 c, d was produced by the reconnection between the twisted lines formed in the NLFFF (shown in Fig. 9 a); which is reminiscent of the tether-cutting reconnection shown in Fig. 3 e. The small inset shown in Fig. 9 c shows the contour of one twist superimposed on the B _z map, where the footpoints for the part of the selected field lines plotted in Fig. 9 c, d are anchored inside this contour. Note that there is no guarantee that this new state can remain in equilibrium because a flux tube composed of strongly twisted lines can escape from the solar surface (Amari et al. 2000; Kusano et al. 2012; Kliem et al. 2013).

Next, an MHD simulation was executed using this new state, as shown in Fig. 9 c; note that at the boundary, all components of the velocity are fixed to zero, and the normal component of B is fixed, while the horizontal one may vary, i.e., it is determined by the induction equation according to the dynamics. Consequently, as shown in Fig. 10, the equilibrium was broken, and a larger flux tube was formed and launched into the upper corona. Note that, in this process, the strongly twisted lines (in orange) that were formed during the initial state do not extend directly into the upper corona. Rather, they reconnect with the ambient field lines (in blue) that convert into the large flux tube. Interestingly, the strongly twisted lines in the initial state appear to convert into the post-flare loops often observed after a flare.

These simulation results were compared with observations. The authors first confirmed that their simulation captures the shape of the two-ribbon flares. Following the CSHKP model, two-ribbon flares are generally considered to be due to the distribution of the footpoints of the reconnected field lines. Therefore, those could be reproduced to trace the reconnected field lines during a simulation. To achieve this, the authors traced the reconnected field lines by using the following equation:

$$\delta(\boldsymbol{x}_{0},t_{n}) = |\boldsymbol{x}_{1}(\boldsymbol{x}_{0}, t_{n+1}) - \boldsymbol{x}_{1}(\boldsymbol{x}_{0}, t_{n})|, $$

where t _n+1 is the next time step after t _n, and x ₁(x ₀,t _n) is the location of one footpoint of each field line at time t _n, which is traced from another footpoint at x ₀. Eventually, we calculate

$$ \Delta(\boldsymbol{x}_{0},t) = {\int_{0}^{t}} \delta(\boldsymbol{x}_{0},t_{n}){dt}_{n}, $$

(60)

where Δ(x ₀,t) is a location where the length of a field lines is changed, meaning that the enhanced region corresponds to one in which there was a dramatic reconnection in the twisted lines. Figure 11 a shows a 3D view of the field lines at t = 4.0, when the large flux tube has been formed during the initial launching phase. We first confirmed that the sheared two-ribbon profiles observed initially were reproduced in our simulation. Figure 11 b shows the two-ribbon flares during the X2.2-class flare, observed by Hinode/SOT, at 01:50 UT, corresponding to the initial phase of the flare. Figure 11 c shows the numerically calculated two-ribbon flares, following Eq. (60), at t = 4, reproduced in this simulation where Δ is chosen from the region in which T _n>0.3. The shape of the numerically calculated two-ribbon flares matches the observed one.

These simulation results were further compared with the EUV image data obtained from SDO/AIA. Figure 11 d shows the 3D magnetic structure at t = 15, clearly revealing the post-flare loops above which the large eruptive flux tube is ascending. We confirmed that the post-flare loops can capture the field lines in the EUV image, using simulation data at t= 15. Figures 11 e shows the EUV image observed after the flare by 94 Å of SDO/AIA, and Fig. 11 f shows the field lines at t = 10 superimposed on the EUV image. The field lines observed in the EUV image were successfully captured.

Finally, enhancement of the horizontal magnetic field B _t was discussed by Inoue et al. (2015). As shown in Fig. 12 a, Wang et al. (2012) found a rapid enhancement of the horizontal field on the PIL in the photosphere, and they suggested that this was due to the reconnection. The simulation of Inoue et al. (2015) also indicated this enhancement, and the result is shown in Fig. 12 c calculated for the area shown in Fig. 12 b. It was pointed out that the post-flare loops can be observed even during an early phase in which the horizontal fields are enhanced, and the new post-flare loops are subsequently produced through the above reconnection. Consequently, it was suggested that this enhancement is due to the accumulation of post-flare loops suppressing the pre-existing loops. Therefore, this enhancement would be strongly related to the reconnection. However, since this simulation was performed in the zero-beta MHD, to support this conclusion, it is necessary to have a more detailed analysis and discussion under more realistic assumptions, including high- β regimes corresponding to the chromosphere and the photosphere.

A summary of the dynamics is shown in Fig. 13. (i) The NLFFF is quite stable for the current-driven ideal MHD instability, so it is necessary to have a trigger process (here, the tether-cutting reconnection) to break the equilibrium. (ii) The tether-cutting reconnection creates strongly twisted lines in the NLFFF. Consequently, it breaks the equilibrium and reconnects with the ambient field lines. The result is that a large flux tube is formed as it ascends. (iii) Eventually, the flux tube will grow into a CME if the threshold of the torus instability is exceeded or equilibrium is lost.

Conclusions

The solar physics satellites Hinode and SDO, together with modern ground-based telescopes, provide photospheric magnetic field data with unprecedented accuracy. This enables us to reconstruct the 3D coronal magnetic field with high accuracy, such that it includes the potential field from the normal component not only of the photospheric magnetic field but also of the NLFFF, which contains both the normal and the horizontal magnetic fields. Because the NLFFF is reconstructed to include information about the horizontal magnetic fields at the photosphere, it can yield a 3D magnetic field close to that observed in the active regions instead of the one similar to that of the potential field, and it can show the accumulation of free magnetic energy and helicity that is required to produce a flare. In addition, the force-free α is given as a function of space, and so it is not an LFFF approximation. Therefore, the NLFFF can yield the magnetic configuration both before and after the flare, and several papers have reported various important physical quantities obtained from the NLFFF, including the free magnetic energy (Sun et al. 2012; Jiang et al. 2014b), the magnetic helicity (Thalmann et al. 2011; Valori et al. 2012; Pevtsov et al. 2014), and the magnetic twist and topology (Inoue et al. 2011; Guo et al. 2013; Inoue et al. 2013; Zhao et al. 2014). These quantities quantify the NLFFF stability, which cannot be obtained from observations.

On the other hand, there is a problem in the NLFFF itself. Using the same format as in Fig. 5 d, Fig. 14 shows the distribution of the force-free α measured at both footpoints of each field line for the NLFFF in Fig. 7 b and the temporal evolution of $\int |\mathbf {\nabla } \cdot \boldsymbol {B}|^{2}$dV during the iteration of the NLFFF. Although the value of $\int |\mathbf {\nabla } \cdot \boldsymbol {B}|^{2}$dV is reduced to fourth order, the distribution of the force-free α is scattered. Therefore, an unexpected physical element, the residual force, remains; this is inevitably produced near the boundary in the NLFFF, due to the contradiction between the boundary and the inner domain. In addition, it should be noted that the coronal magnetic fields cannot be correctly reproduced only by the NLFFF. Peter et al. (2015) pointed out several limitations on the free energy and accumulated currents. Furthermore, reconstruction of the geometry of bright loops requires methods more advanced than the NLFFF (Aschwanden et al. 2014; Malanushenko et al. 2014). Therefore, a model more advanced than the NLFFF is required to construct the equilibrium state with high accuracy and overcome these limitations.

Although the NLFFF yields the 3D properties of the magnetic field, this method does not reveal the dynamics of the solar flares. To determine the dynamics in a realistic situation, NLFFF results have been used as initial conditions for MHD simulations (Jiang et al. 2013; Kliem et al. 2013; Inoue et al. 2014a; Amari et al. 2014; Inoue et al. 2015). Because these simulations were constrained by the photospheric magnetic field, there are large artificial processes causing the buildup of energy; these likely yield twist and sheared motions, which were not assumed. Important and realistic physical processes are also being revealed, including the critical value for the flux of the flux tube for an eruption (Kliem et al. 2013) or the formation of a large flux tube producing a CME (Inoue et al. 2014a; 2015). Furthermore, the reliability of these simulations can be confirmed because they can be more precisely compared with the observations likely by Inoue et al. (2014a) and Inoue et al. (2015), in contrast to previous simulations that described hypothetical situations. Note that several can be indirectly compared, e.g., the two-ribbon flares discussed in this study. In order to provide a strict confirmation, however, a direct comparison is required (e.g., (Mikić et al. 2013)).

Some problems and questions related to these simulations still remain to be answered. For instance, as discussed above, the reconstructed field does not completely achieve a force-free state, and so the residual force must be treated carefully. If these residual forces are sufficiently strong, they may affect the magnetic field dynamics, and the interpretation of the dynamics becomes difficult. In addition to this, as Inoue et al. (2015) pointed out, the magnetic twist accumulated in the NLFFF might be gradually reduced throughout the numerical diffusion and also on the solar surface because the NLFFF returns to a lower energy level without retaining the observed horizontal magnetic fields. Furthermore, it is important to account for the observed process that triggers the solar flares in order to understand the conversion of the stable magnetic field into a dynamic one. Recently, the triggering was observed by using state-of-art data (e.g., Green et al. (2011); Bamba et al. (2013); Louis et al. (2015)). These data must be incorporated into simulations. Although most simulations start from an NLFFF that is already composed of twisted and sheared field lines, some studies attempted to recover the processes leading from the buildup to the release of energy; in this data-driven simulation, the coronal magnetic field was driven by the time-dependent photospheric magnetic field e.g., Cheung and De Rosa (2012). Work in this direction is currently underway, and this will be extended in the future.

With advanced computational resources now more readily available, more-refined 3D numerical MHD models of solar eruptions are being developed and improved. Recently, techniques combining simulations with highly resolved temporal and spatial data from state-of-the-art solar satellites have been developed, and these have yielded some preliminary results. In the future, it is likely to be necessary to further develop simulations of solar flares in order to more closely correspond to these observations.

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Acknowledgements

We thank the Japan Geoscience Union (JPGU) for inviting us to the JPGU 2014 meeting. We are grateful to the referees for providing many constructive comments and for suggesting ways in which to improve this paper. We are grateful to one of the science editors, Dr. Tsutomu Nagatsuma, for encouraging us, and to the MPS members for useful discussions. We offer special thanks to Dr. Takahiro Miyoshi and Dr. Vinay Shankar Pandey for checking a part of this paper. S. I. thanks the Alexander Von Humboldt Foundation for supporting our work and for providing a precious opportunity to work in Germany. This work was also supported by JSPS KAKENHI Grant Number 15H05814 (PI: K. Kusano). The computational work was carried out within the computational joint research program at the Institute for Space-Earth Environmental Research, Nagoya University. The computer simulation was performed on the Fujitsu PRIMERGY CX400 system of the Information Technology Center, Nagoya University. Visualization was performed by VAPOR (Clyne and Rast 2005; Clyne et al. 2007). Finally, S. I. sincerely thanks Professor Kanya Kusano for providing an opportunity to engage in this work and for many constructive comments and discussions.

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Max-Planck Institute for Solar System Research, Justus-von-Liebig-Weg 3, Göttingen, 37077, Germany
Satoshi Inoue
Institute for Space-Earth Environmental Research, Nagoya University, Chikusa-ku, Furo-Cho, Nagoya, 446-701, Japan
Satoshi Inoue

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Inoue, S. Magnetohydrodynamics modeling of coronal magnetic field and solar eruptions based on the photospheric magnetic field. Prog. in Earth and Planet. Sci. 3, 19 (2016). https://doi.org/10.1186/s40645-016-0084-7

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Received: 15 December 2014
Accepted: 28 March 2016
Published: 04 July 2016
DOI: https://doi.org/10.1186/s40645-016-0084-7

Keywords

Sun
Magnetic field
Photosphere
Corona
Magnetohydrodynamics (MHD)
Solar active region
Solar flare
Coronal mass ejection (CME)