A&A 477, 649-655 (2008)
DOI: 10.1051/0004-6361:20078266

Dynamics of plasmoids formed by the current sheet tearing

M. Bárta1 - B. Vrsnak2 - M. Karlický1


1 - Astronomical Institute of the Academy of Sciences of the Czech Republic, 25165 Ondrejov, Czech Republic
2 - Hvar Observatory, Faculty of Geodesy, Kaciceva 26, 10000 Zagreb, Croatia

Received 13 July 2007 / Accepted 28 September 2007

Abstract
Context. Moving blob-like features observed in the soft X-ray and EUV range above flare-loops are often interpreted as signatures of plasmoids formed by the current sheet tearing in the flare-associated reconnection process.
Aims. We investigate the evolution of the flare-associated current sheet numerically in order to analyse the kinematics and dynamics of plasmoids. The goal is to explain the broad diversity of kinematical properties of the plasmoid signatures recorded by various observational techniques.
Methods. We performed a 2-dimensional resistive-MHD numerical simulation of the reconnection starting from the Harris-type current sheet. After identifying the plasmoids, we followed their motion to determine basic kinematical parameters (velocity and acceleration), and we analysed the associated magnetic field topology.
Results. The simulation reveals a broad variety of the kinematical/dynamical properties of plasmoids - after formation, a plasmoid can move upward, downward, or can even change its direction of propagation. The highest velocities, in the range of the ambient Alfvén speed, are found in the case of upward propagating plasmoids. The acceleration is determined by the net magnetic field tension of the reconnected field lines. Downwardly propagating plasmoids achieve only a fraction of the ambient Alfvén speed. They strongly decelerate during the coalescence with low-lying flare-loops, when distinct energy-release peaks occur and loop system oscillations are excited.
Conclusions. The presented results explain, qualitatively and quantitatively, the broad spectrum of kinematical properties of various observational features attributed to the current-sheet plasmoids.

Key words: Sun: flares - Sun: corona - magnetohydrodynamics (MHD) - methods: numerical

1 Introduction

The eruption of a coronal mass ejection (CME) is supposed to be associated with the formation of a large-scale vertical current sheet (CS) between the CME body and the solar surface: e.g., Lin (2004), Riley et al. (2007); for the observational aspect see, e.g., Vrsnak et al. (2002), Ko et al. (2003) Bemporad et al. (2006). The length of the CS increases in time due to the outward propagation of the CME, and when its length-to-width ratio becomes high enough, tearing instability sets in (Furth et al. 1963; Ugai 1987; for the observational aspect see Vrsnak et al. 2003). The X-type neutral line forms along the CS, becoming the heart of fast reconnection in the erupting magnetic field arcade. Reconnection results in a growing system of post-eruption loops, and if the reconnection-associated electric fields are strong enough to accelerate sufficient number of non-thermal particles (for various mechanisms of particle acceleration see, e.g., Aschwanden 2002), the loops become the site of a solar flare.

As the CS elongates, it is more and more likely that two (or more) X-lines form, and in between a plasmoid(s) is created (e.g., Schumacher & Kliem 1997). This is a common feature in 2-D numerical simulations of the two-ribbon flare reconnection (for 3-dimensional effects of the plasmoid formation and evolution, see Vrsnak 2003). Most often, such numerical studies are focused mainly on the coalescence of small-scale plasmoids to explain the fragmentation of the flare's energy release (Kliem et al. 2000; Shibata & Tanuma 2001), or on the upward ejected plasmoids, aiming to explain the CME process itself (see, e.g., Ugai 1992). However, we note that Forbes & Priest (1983) already recognised the downward-moving plasmoids.

The plasmoid concept is frequently used to interpret various observational phenomena from X-rays to radio waves. In the soft X-ray (SXR) range, upward-moving blobs of hot plasma are frequently observed (e.g., Shibata et al. 1995; Ohyama & Shibata 1998; Kundu et al. 2001; Kim et al. 2005, and references therein). White-light coronagraphic observations frequently reveal rising blob-like features in "rays'' formed in the wake of CMEs (Ko et al. 2003; Lin et al. 2005) or downward-moving structures in the region above the post-eruption loop system (Sheeley & Wang 2002; for a similar phenomenon observed in SXR and EUV see MacKenzie & Hudson 1999; McKenzie 2000; Raymond et al. 2003). Slowly drifting pulsating-structures sometimes observed in the microwave-wavelength dynamic spectra are often interpreted as a signature of upward or downward moving plasmoids (Kliem et al. 2000; Karlický 2004; Karlický & Bárta 2007; Ning et al. 2007).

In this paper we perform a detailed analysis of the kinematics of current-sheet plasmoids, employing numerical magnetohydrodynamical (MHD) simulations. In Sect. 2 we briefly describe the model and numerical procedure (details are provided in the Appendix; see also Bárta et al. 2007). In Sect. 3 we analyse the kinematics of plasmoids in various situations. The dynamics of the plasmoid motion is interpreted and discussed in Sect. 4, and the conclusions are drawn in Sect. 5.

2 The model

The simulation is based on the standard set of 2-dimensional (2D) MHD equations, with the resistivity dependent on the electric current density (see Appendix). The initial configuration is a symmetric Harris-type CS coaligned with the y-axis, which is set in the middle of the 2D rectangular computation domain (Fig. 1). We use dimensionless variables for convenience throughout the simulation: the spatial coordinates x and y are expressed in units of the initial CS width $L_{\rm A}$ and time in units of the Alfvén transit time $\tau_{\rm A}=L_{\rm
A}/v_{\rm A0}$, where $v_{\rm A0}=B_0/\!\sqrt{\mu_0\rho_0}$ is the asymptotic value ( $x\rightarrow\infty$) of the Alfvén speed at t=0 (see papers by Karlický 1988; and Kliem et al. 2000, for details). In the following, we denote by v the velocity normalised to the Alfvén velocity $v_{\rm A0}$, whereas by a we denote the dimensionless acceleration, expressed in units of $v_{\rm A0}/\tau_{\rm A}$, i.e., $v_{\rm A0}^2/L_{\rm A}$. The ratio of specific heats is chosen to be $\gamma=2$, and the initial asymptotic value of plasma-to-magnetic pressure ratio is set to $\beta=0.15$.

At t = 0, a limited area at the coordinate-system origin is perturbed by anomalous resistivity to initiate reconnection. It results in plasma inflow from both sides of the CS, which leads to its compression. As a consequence, around $t \approx 250 \tau_{\rm A}$ the dissipative region (an X-type neutral point; hereinafter X-point) moves rapidly from the origin to a new location at $y
\approx 10 L_{\rm A}$ (see also Karlický & Bárta 2006). This change of magnetic field topology is associated with a distinct peak of dissipation power (see the bottom panel of Fig. 1; for definition see Appendix). After this transient stage, a long period of quasi-stationary Petschek-like regime of reconnection is established, lasting from $t \approx 300 \tau_{\rm A}$ to $1000\tau_{\rm A}$ (see the smooth part of the dissipation power profile at the bottom of Fig. 1). During this period the newly formed loop system slowly grows (the X-point moves upward) as a consequence of newly reconnected magnetic flux, being "rooted'' at the bottom boundary ( vx(x, 0) = 0). This behaviour is consistent with general flare models, as well as with observations. The final phase of the computation ( $t \gtrsim 1000 \tau_{\rm A}$) is highly intermittent, due to formation of a number of plasmoids. The dissipation power shows numerous peaks, each caused either by mutual coalescence of plasmoids or by coalescence of plasmoids with the underlying loop system (see the bursting part of the dissipation power profile; for detailed discussion see Bárta et al. 2007).


  \begin{figure}
\par\includegraphics[width=16cm,clip]{8266fig1.eps} \end{figure} Figure 1: The first three rows show an upward-moving plasmoid, downward-moving plasmoid, and a pair of upward-moving plamoids and their coalescence. Magnetic field lines are presented by dashed lines on the grayscale background representing the density; the field lines outlining the plasmoids are enhanced by bold lines (schematically presented in Fig. 7). The time profile of the dissipation power is presented in the bottom panel.
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3 Kinematics of plasmoids

3.1 Upward motion of an isolated plasmoid

In Fig. 2 the upward propagation of the plasmoid formed around $t=1030~\tau_{\rm A}$ at $y=54~L_{\rm A}$ is presented (see also 1st row of Fig. 1). The accuracy of the measured positions of the plasmoid centroid and its leading and following edge is $\Delta y=0.2~L_{\rm A}$. The velocity estimates are based on $\Delta t=10~\tau_{\rm A}$ intervals, so the velocities determined from two successive position measurements have an accuracy of $\Delta v=0.02~v_{\rm
A0}$.

As expected, the plasmoid velocity is close to the external Alfvén speed: the mean velocity of the plasmoid estimated by the linear least-square fit equals $\overline v= 0.96~v_{\rm A0}$ (see inset in Fig. 2). However, we note that the plasmoid centroid, in fact, does not move uniformly but shows acceleration. The mean value estimated by using the 2nd degree polynomial least-square fit equals $\overline a\approx 0.006~v_{\rm A0}/\tau_{\rm A}$.

3.2 Downward-propagating plasmoids

Beside upward-propagating plasmoids, our simulation reveals downward-moving plasmoids, too. In Fig. 3 the downward propagation of the plasmoid formed at $y=47~L_{\rm A}$ around $t=1060~\tau_{\rm A}$ (see 2nd row in Fig. 1) is presented. Obviously, the motion is more complex than in the case of freely upward-propagating plasmoid: there is an acceleration phase, followed by a phase of approximately constant velocity, and finally, strong deceleration occurs before the plasmoid loses its identity in coalescence with the flare-loops.

The maximum velocity reached is $v\approx0.65~v_{\rm A0}$. The initial-phase acceleration is of the order of $\overline a\approx 0.01~v_{\rm A0}/\tau_{\rm A}$. Strong deceleration begins after the interaction with the low-lying flare loops has started. The interaction is revealed by deformation of the X-point structure between the plasmoid and loops. The X-point transforms into a small horizontal CS, characterised by an intense reverse current. The deceleration is especially rapid at the frontal edge of the plasmoid; e.g., the X-point decelerates at $\overline a\approx
-0.03~v_{\rm A0}/\tau_{\rm A}$. On the other hand, the centroid decelerates at $\overline a\approx
-0.025~v_{\rm A0}/\tau_{\rm A}$ and such a non-uniform deceleration causes a deformation of the plasmoid shape. The mean velocity over the distance from $y=47~L_{\rm A}$ to $y=21~L_{\rm A}$(t=1080-1150  $\tau_{\rm A}$) equals $\overline v=0.4~v_{\rm A0}$.

3.3 Complex propagation

In Fig. 4 we present a complex propagation of the plasmoid formed at $y=47~L_{\rm A}$around $t=1150~\tau_{\rm A}$. The plasmoid initially moves upward at the velocity $v=0.3~v_{\rm
A0}$, showing a deceleration of $\overline a=-0.007~v_{\rm A0}/\tau_{\rm A}$. After achieving the maximum height $y=56~L_{\rm A}$, it starts to accelerate downwards at $\overline a=0.004~v_{\rm
A0}/\tau_{\rm A}$ and achieves the highest velocity of $v=0.35~v_{\rm A0}$. Finally, after the onset of the interaction with low-lying flare loops, the plasmoid decelerates at $\overline
a=-0.01~v_{\rm A0}/\tau_{\rm A}$, until it stops and loses its identity at $y\approx26~L_{\rm
A}$. The evolution of the reverse current formed in the interaction of the plasmoid and flare-loops, and the associated plasmoid deceleration are qualitatively similar to that described in Sect. 3.2. However, the deceleration is considerably weaker in this case.

3.4 Coalescing plasmoid pairs

In Fig. 5 we present kinematics of two plasmoids that coalesce above the flare loops. Initially, both plasmoids move upward at $v\approx v_{\rm A0}$. The phase lasting from t=1500 to 1520  $\tau_{\rm A}$ is characterised by the accelerated merging motion towards the X-point between the plasmoids. The leading plasmoid decelerates by $a=-0.01~v_{\rm A0}/\tau_{\rm A}$ and the following one accelerates by $a=+0.008~v_{\rm A0}/\tau_{\rm A}$. The X-point in between them moves at approximately constant velocity of $v\approx v_{\rm A0}$.

During the coalescence phase, the X-line located between plasmoids transforms: the reconnection of the magnetic field bounding the CS stops, because the merging motion of plasmoids reduces the length-to-width ratio of the CS segment between them. After the plasmoids come close enough, the secondary CS is induced between them. In this small CS (characterised by the reverse current), the reconnection of the poloidal fields of plasmoids starts, driven by the attractive force of the parallel currents flowing along the plasmoids. This phase lasts from t=1520 to 1530  $\tau_{\rm A}$, during which the plasmoids lose their individuality. After $t=1530~\tau_{\rm A}$ the newly formed plasmoid continues to move upward at the velocity $v\approx v_{\rm A0}$. After $t\approx
1550~\tau_{\rm A}$, a complex motion similar to what is shown in Fig. 4 is observed ( $a\approx -0.007~v_{\rm A0}/\tau_{\rm A}$), but characterised by a faster descending motion, $v\approx 0.9~v_{\rm A0}$. The final deceleration of the plasmoid is around $\overline
a=-0.01~v_{\rm A0}/\tau_{\rm A}$.


  \begin{figure}
\par\resizebox{8.8cm}{!}{\includegraphics{8266fig2.eps}}
\end{figure} Figure 2: Kinematics of the upward-propagating plasmoid formed at $t\approx1030~\tau_{\rm A}$. The motion of the centroid is presented (bold line), together with the leading and following edge (thin lines). The linear least square fits are shown in the inset.
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  \begin{figure}
\par\resizebox{8.8cm}{!}{\includegraphics{8266fig3.eps}}
\end{figure} Figure 3: Kinematics of the downward propagating plasmoid formed around $t=1060~\tau_{\rm A}$. Positions of the centre of the plasmoid (bold line) and the X-point below the plasmoid (thin line) are shown.
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  \begin{figure}
\par\resizebox{8.8cm}{!}{\includegraphics{8266fig4.eps}}
\end{figure} Figure 4: Kinematics of the plasmoid formed around $t=1150~\tau_{\rm A}$. Positions of the centroid (bold line) and the X-points below and above the plasmoid (thin lines) are shown.
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  \begin{figure}
\par\resizebox{8.8cm}{!}{\includegraphics{8266fig5.eps}}
\end{figure} Figure 5: Kinematics of a pair of plasmoids formed around $t=1460~\tau_{\rm A}$. The positions of centroids and the X-points are shown by bold and thin lines, respectively. The coalescence phase is indicated; at this stage, it was not possible to identify precisely the plasmoid centroids, i.e., there is no well-defined position information.
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3.5 Characteristics of the reconnection outflows


  \begin{figure}
\par\resizebox{8cm}{!}{\includegraphics{8266fig6.eps}}
\end{figure} Figure 6: The outflow speed uy (dashed line) and the magnetosonic Mach number $M_{\rm ms}$ (full line) measured along the y-axis at $t=300\tau _{\rm A}$.
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The presented analysis demonstrates that plasmoids show a broad variety of kinematical behaviours. Bearing this in mind, it is instructive to check outflow velocities in the steady-state reconnection regime ($t \approx$ 300-1000  $\tau_{\rm A}$), representing a kind of the referent velocity pattern. In Fig. 6 we show the plasma flow velocity uy(y) and the corresponding magnetosonic Mach number $M_{\rm ms}$, measured along the y-axis.

Inspecting Fig. 6, we find several differences between the upward and downward jets, which are separated by the diffusion region centred around $y
\approx 10 L_{\rm A}$, where uy=0. The upward jet consists of a flow-acceleration segment ($y\approx$ 10-15 $L_{\rm A}$) and the constant-velocity segment ( $y\gtrsim20$ $L_{\rm A}$) characterised by the velocity $u_y\approx$ 0.9-1  $v_{\rm A0}$. Such outflow velocities are consistent with the analytical reconnection theory (see, e.g., Appendix in Aurass et al. 2002). On the other hand, the downward jet, being squeezed between the diffusion region and the flare loops, consists of the acceleration segment ($y\approx$ 10-8 $L_{\rm A}$) and the deceleration segment ($y\approx$ 8-7 $L_{\rm A}$). The velocity never exceeds 0.75  $v_{\rm A0}$, so flow velocities, similar to plasmoid velocities, tend to be higher in the upward than in the downward jet.

It is interesting to note that, although the upward and downward outflow velocities are quite different, the maximum magnetosonic Mach numbers are relatively similar, ranging around 0.6 and 0.7 for the downward and upward jets, respectively. Thus, both jets are submagnetosonic and have comparable Mach numbers. Such an outcome differs from simulations performed by Forbes (1986) and Forbes & Malherbe (1991), where it was found that flow velocities in the upward and downward jets are comparable only if the upward jet is supermagnetosonic. According to these simulations, the downward outflow does not exist if the upward jet is submagnetosonic. It is quite likely that our reconnection regime is somewhere in between these two situations, but it should be also emphasised that the simulations differ in several physical and technical details (e.g., energy equation, numerical resistivity, etc.).

Finally, it should be noted that, for the ratio of specific heats $\gamma=2$, which we used in the simulation, one would expect from the analytic theory that reconnection outflows are supermagnetosonic already for $\beta<0.5$ (see, e.g., Eq. (39) of Forbes & Malherbe 1991). In other words, according to the analytic theory, our jets should be supermagnetosonic, since we used $\beta=0.15$. Such a discrepancy is inherent in comparisons of the analytical and numerical results. For example, Forbes & Malherbe (1991) found that outflows become supermagnetosonic for $\beta<0.2$, whereas one would expect the limiting value to be $\beta<0.8$, since they used $\gamma=5/3$. A possible explanation might be related to the numerical limitations of simulations; for example, after checking the spatial distribution of $\beta$, we found that its value starts to be well above $\beta=0.15$ already at 0.1-0.2 $L_{\rm A}$, upstream of the slow mode shocks.

4 Interpretation and discussion

4.1 Direction of motion


  \begin{figure}
\par\resizebox{8cm}{!}{\includegraphics{8266fig7.eps}}
\end{figure} Figure 7: Schematics of the magnetic field pattern when the plasmoid moves: a) upward, b) downward (compare with Fig. 1). Horizontal arrows depict the magnetic-flux inflow rate at the diffusion region above (v1B1) and below (v2B2) the plasmoid. Vertical arrows indicate the direction of the plasmoid motion.
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The basic question that arises from the presented analysis is what conditions determine the direction of the plasmoid motion. Since the magnetic tension of the reconnected field lines is the primary driver of the plasma motion in the reconnection outflow jet (the "sling-shot effect''; see, e.g., Vrsnak & Skender 2005), we compare the magnetic field-line pattern in situations of upward and downward motion. In Fig. 7a we sketch the pattern we find in the case of upward-moving plasmoids (note the V-shape of field lines around the plasmoid, giving rise to the upward directed tension), whereas in Fig. 7b we show the pattern corresponding to downward moving plasmoids (the inverse V-shape of field lines results in downward-directed tension).

The primary parameter that governs the described shapes of field lines is the reconnection rate $\vec{v}\times\vec{B}$ at X-points above and below the plasmoid. If $\vec{v}\times\vec{B}$ is higher at the X-point above the plasmoid than at the X-point below it, i.e., if the rate by which the magnetic flux is reconnected in the upper diffusion region is higher than in lower one, the field lines form a pattern like in Fig. 7b and the field line tension drags the plasmoid downwards. If more field lines are reconnected in the lower diffusion region than in the upper one, the resulting pattern is like in Fig. 7a and the plasmoid is expelled upwards.

Especially interesting are situations when the direction of motion changes (Fig. 4, as well as Fig. 5 after the coalescence). Indeed, in these cases the topology of field lines changes from that drawn in Fig. 7a into what is shown in Fig. 7b (e.g., around $t=1165~\tau_{\rm A}$ the pattern is like in Fig. 7a, and around $t=1215~\tau_{\rm A}$ the pattern is like in Fig. 7b). Such a transformation implies a change in the reconnection rate in both the upper and lower diffusion region; i.e., the magnetic flux inflow increases above the plasmoid and decreases below it. In this respect, note that the rate at which magnetic flux flows into the CS generally depends on the position, i.e., the y-coordinate; it fluctuates around the steady-state conditions due to MHD waves created in the interaction of the downward directed reconnection jet (and imbedded plasmoids) with the flare loops, as well as due to perturbations left behind the previous upward and/or downward moving plasmoids.

4.2 Accelerations and velocities

The acceleration of the CS outflow, i.e., the existence of the fast outflow jets in the reconnecting CS, is a consequence of the magnetic field tension of strongly bent reconnected field lines. The equation of motion can be written in an approximate form:

\begin{displaymath}\rho \hat a=\frac{B_x}{\mu_0}\frac{\partial B_y}{\partial x} \approx \frac{M_{\rm Ai}}{\mu_0}\frac{B_y^2}{L_{\rm A}},
\end{displaymath} (1)

where $\hat a$ is the acceleration expressed in m s-2, $\rho$ the mass density, Bx and By are the x and y components of the magnetic field, $M_{\rm Ai}$ the inflow Afvénic Mach number, and we used $B_x/B_y \approx M_{\rm Ai}$ (Soward & Priest 1982; Aurass et al. 2002; for a complete treatment see Skender et al. 2001). Consequently, $a\approx M_{\rm Ai} v_{\rm Ai}^2/L_{\rm A}$, i.e., $a\approx M_{\rm Ai} v_{\rm A0}/\tau_{\rm A}$, since the Alfvén speed in the inflow plasma is $v_{\rm Ai}\approx v_{\rm A0}$ and $\tau_{\rm A}=L_{\rm
A}/v_{\rm A0}$. As a result, the highest values of the acceleration should be of the order of a=0.01-0.02  $v_{\rm A0}/\tau_{\rm A}$, since after $t\approx 600~\tau_{\rm A}$the inflow Mach number varies between $M_{\rm Ai}\approx 0.01$ and 0.02 (Bárta et al. 2007). Note that these values of $M_{\rm Ai}$ are consistent with the empirical values inferred by Bemporad et al. (2006).

The accelerations found in Sect. 3 are in the range $\vert\overline
a\vert=0.005$-0.01  $v_{\rm A0}/\tau_{\rm A}$; i.e., they are somewhat smaller than calculated, probably because the CS thickness at the plasmoid location is larger than $L_{\rm A}$. Taking the order of magnitude values $v_{\rm A0}=1000$ km s-1 and $L_{\rm A}=1000$ km (see the Appendix for details), which is equivalent to $\tau_{\rm A}=1$ s, this corresponds to $\vert\overline a\vert=5$-10 km s-2. If we compare this order of magnitude estimate with Kim et al. (2005), who measured in three SXR plasmoids a strong acceleration of about 2.5, 1.3, and 2 km s-2, we find that our result is consistent with the SXR observations if we assume $v_{\rm A0}=500$ km s-1, which is a reasonable value for the active region corona (see, e.g., Vrsnak et al. 2004).

Our simulation shows that plasmoids achieve a wide range of velocities, with an upper limit around $v\approx v_{\rm A0}$. This is consistent with the SXR observations that usually reveal velocities from several tens to several hundred km s-1 (e.g., Shibata et al. 1995), rarely exceeding 1000 km s-1 (Kim et al. 2005). Somewhat lower velocities are observed in downflows (McKenzie & Hudson 1999; McKenzie 2000), as we also found in our simulation.

In this respect, it is interesting to note that the blob-like features recorded by coronagraphs (Ko et al. 2003; Lin et al. 2005), presumably representing plasmoids at greater heights, show similar velocities but considerably weaker accelerations (below 100 m s-2; Ko et al. 2003) than SXR plasmoids. Lower accelerations are probably a consequence of a larger CS width and weaker ambient field at greater heights, resulting in a weaker tension. On the other hand, velocities are similar, since in the considered height range the Alfvén velocity does not change very much (Vrsnak et al. 2004). The downward propagating coronagraphic plasmoids again show a somewhat lower velocities, generally below 100 km s-1 (Sheeley & Wang 2002).

4.3 Interaction with flare loops

The deceleration of downward-directed plasmoids in the stage of coalescence with flare loops is especially important, since these intervals correspond to the most powerful energy-release episodes (Bárta et al. 2007). During the coalescence the "reverse'' current is induced, causing strong deceleration of the plasmoid: since the merging speed is higher than the diffusion velocity, the magnetic field piles up, which leads to the magnetic pressure increase between the flare-loops and the plasmoid. Due to the strong "collision'', the plasmoid and flare-loops get deformed. As a result, large amplitude waves are excited, propagating downward along outermost loops in the system. After the coalescence, eigenmode oscillations in the loop system develop (to be analysed in a separate paper).

Interactions of plasmoids with the flare loops, as well as plasmoid-plasmoid interactions, are also important from the point of view of the flare energetics. Each time the plasmoid-loop or the plasmoid-plasmoid coalescence occurs, we find a prominent sharp peak in the dissipation-power curve, as can be seen in the bottom panel of Fig. 1. It is interesting to note that the plasmoid-loop coalescence should have a distinct observational signature. Since the plasmoid interacts with the field lines that map the part of the flare ribbon that is already behind the frontal edge of the ribbon, the plasmoid-loop coalescence should be seen as re-brightening of certain parts of the flaring area. Such a phenomenon might be difficult to observe in chromospheric spectral lines, which are often burdened by saturation effects. On the other hand, it might explain re-brightenings of certain footpoint sources sometimes observed in hard X-rays (see, e.g., Miklenic et al. 2007).

5 Conclusion

The current-sheet tearing results in formation of plasmoids whose dynamics is determined by the reconnection rate at the two associated X-points. If the reconnection rate is higher at the X-point located below the plasmoid, the plasmoid moves upward since the net tension causes the upward acceleration. If the reconnection is faster at the X-point above the plasmoid, it accelerates downward. The accelerations are limited $\vert a\vert<M_{\rm Ai}v_{\rm A0}/\tau_{\rm A}$. For the ambient Alfvén velocity of the order of 1000 km s-1, the dimensionless reconnection rate $M_{\rm
Ai}=0.01$, and the effective CS thickness of 1000 km (Shibata & Tanuma 2001; Lin et al. 2007), the upper limit to the acceleration equals to a=10 km s-2. This upper limit is consistent with the observed accelerations of upward-moving SXR plasmoids, which attain values of several km s-2 (Kim et al. 2005).

The upper limit to the plasmoid velocity found in our simulation for the upward propagating plasmoids is consistent with the analytical-approach limit $v\approx v_{\rm A0}$ (see Appendix in Aurass et al. 2002). It is also consistent with observations which do not show significant difference of the plasmoid velocities in the heliocentric distance range R=2-10, where the Alfvén speed is in the range 300-600 km s-1 (see Fig. 3 in Vrsnak et al. 2004).

The downward-moving plasmoids are characterised by lower velocities (only a fraction of $v_{\rm A0}$), since they do not have enough time to accelerate to full speed. The acceleration is stopped by the coalescence of the plasmoid and the low-lying flare loops. After the interaction starts, the plasmoid experiences a strong deceleration as a result of the magnetic flux pile-up between the plasmoid and the loops (the motion is faster than the reconnection velocity), so the mean velocity of the downward-moving plasmoids is significantly lower than the Alfvén speed, which might explain relatively low velocities of downward-moving features observed above the flare loops (MacKenzie & Hudson 1999; McKenzie 2000) or post-eruption loops (Sheeley & Wang 2002).

Finally, we note that our simulation run lasts until $t=1570\tau_{\rm A}$. Assuming the effective Alfvén transit time $\tau_{\rm A}=1$ s, this corresponds to $\approx$ 0.5 h. The plasmoid-dominated phase starts after $t\approx1000\tau_{\rm A}$; i.e., our simulation covered some 10 min of this phase, which apparently continues after the end of our run. In this stage, plasmoids have been forming irregularly in 1-2 min intervals. Assuming the Alfvén velocity of 1000 km s-1, that would correspond to the spatial separation of the order of $\approx$100 Mm. Bearing in mind that some plasmoids move downward, this implies a typical separation between upward-moving plasmoids in the low corona of a few 100 Mm, crossing a certain coronal level in several-minute intervals. Analogously, the downward-moving plasmoids and consequent interactions with flare loops should be observed at a similar frequency.

Appendix: The model

We describe the evolution of the magnetised plasma by the compressible resistive one-fluid MHD equations

    $\displaystyle \frac{\partial \rho}{\partial t}+\mbox{\boldmath$\nabla\cdot$ }(\rho\mbox{\boldmath$u$ })=0$  
    $\displaystyle \rho\frac{\partial \mbox{\boldmath$u$ }}{\partial t}+\rho(\mbox{\...
...mbox{\boldmath$u$ }=-\mbox{\boldmath$\nabla$ } p+ \mbox{\boldmath$j \times B$ }$  
    $\displaystyle \frac{\partial \mbox{\boldmath$B$ }}{\partial t}=\mbox{\boldmath$...
...ldmath$u\times B$ })- \mbox{\boldmath$\nabla\times$ }(\eta\mbox{\boldmath$j$ })$  
    $\displaystyle \frac{\partial U}{\partial t}+\mbox{\boldmath$\nabla\cdot S$ }=0,$  

where the energy flux $\mbox{\boldmath$S$ }$ and auxiliary variables (plasma pressure p and current density $\mbox{\boldmath$j$ }$) are defined by the formulae (see, e.g., Kliem et al. 2000):
    $\displaystyle \nabla\times\mbox{\boldmath$B$ }=\mu_0\mbox{\boldmath$j$ }$  
    $\displaystyle U=\frac{p}{\gamma-1}+\frac{1}{2}\rho u^2+\frac{B^2}{2\mu_0}$  
    $\displaystyle \mbox{\boldmath$S$ }=\left(U+p+\frac{B^2}{2\mu_0}\right)\mbox{\bo...
...boldmath$B$ }+\frac{\eta}{\mu_0}\mbox{\boldmath$j$ }\times\mbox{\boldmath$B$ }.$  

Despite the fact that MHD models are not capable of describing the non-ideal effects (resistivity) consistently, they are included phenomenologically by changing the resistivity $\eta$ dynamically to an anomalous value whenever the drift velocity $v_{\rm D}$ exceeds a given threshold $v_{\rm cr}$(Kliem et al. 2000):

\begin{eqnarray*}\eta(\mbox{\boldmath$r$ },t)=\left\{
\begin{array}{lll}
0 : \...
...:\quad
&\vert&v_{\rm D}\vert> v_{\rm cr}.
\end{array} \right.
\end{eqnarray*}


Here we implicitly assume that the onset of anomalous resistivity is caused by the instability of the electron stream forming the electric current at high electron-ion drift velocity. In our simulation, we take $v_{\rm cr}=3.0 v_0$, but note that the outcome of the simulation does not depend significantly on the choice of $v_{\rm cr}$ (Kliem et al. 2000). In this respect we emphasise that in a simulation of the large-scale processes, one cannot resolve the typical width of the dissipative current sheet ($\approx$10 m; Litvinenko 1996). In Sect. 4.2 we have taken the current sheet width to be of the order of $L_{\rm A}=1000$ km (corresponding to the Alfvén travel time of the order of $\tau_{\rm A}=1$ s), to adjust the spatial/temporal scale with the flare characteristics. In other words, the regions where the enhanced resistivity takes place in our model can be interpreted as dissipative regions (smoothed over the grid-cell) in the sense of the fractal reconnection concept proposed by Shibata & Tanuma (2001; see also Lin et al. 2007, and references therein).

At the very beginning of the simulation, the system consists of the symmetric vertical Harris-type current sheet in the middle of the 2D rectangular computation domain. At t=0, a limited area surrounding the origin is perturbed by anomalous resistivity for a short time. Then the evolution is numerically simulated using the 2D Lax-Wendroff scheme with free boundary conditions on upper part and (due to the sheet symmetry) on both the left and right sides.

Symmetric ( Q(y)=Q(-y)) and anti-symmetric ( Q(y)=-Q(-y)) relations are respectively used for quantities (Q) $\rho, u_x, B_y, U$ and uy, Bx at the bottom part of boundary. This choice ensures a vertical magnetic field at the bottom boundary, and it is equivalent to a fixed boundary simulating the presence of the dense solar photosphere.

In order to have a simple quantitative measure of reconnection energetics we use the power dissipated into the Joule heat,

\begin{displaymath}D=\int_{\rm Box} \eta(x,y)j^2(x,y) {\rm d}x {\rm d}y, \end{displaymath}

as a proxy for the reconnection activity.

Acknowledgements
This research was supported by Grant IAA300030701 of the Academy of Sciences and grant 205/07/1100 of the Grant Agency of the Czech Republic. B.V. is grateful to the Astronomical Institute of the Academy of Sciences of the Czech Republic for sponsoring his stay at Ondrejov in 2006. B.V. also acknowledges the support of ISSI-Bern, who sponsored the project "Current Sheet Observations vs. Current Sheet Models'' (P.I. Dr. Giannina Poletto) and provided the organisation of team meetings that played a significant role in motivating this work. We would like to thank to Drs. Alessandro Bemporad, Jun Lin, and Giannina Poletto, as well as an unknown referee, whose comments and suggestions led to significant improvement of the paper.

References

 

Copyright ESO 2007