Chin. Astron. Artrophys. (1995)19/4,459479 A translation of Acta Astron. Sin. (1995)36/2,1Sl-187 Copyright @ 1995 Elsevier Science Ltd Printed in Great Britain. All rights resewed 0275-1062/95$24.00+.00
027%1062(95)00063-l
Flares and separatrices between magnetic 1oopst WANG Jing-xiu
SHI Zhong-xian Beijing Astronomical
Observatory, Chinese Academy of Sciences,
Beijing 100080
WANG Hai-min Big Bear Sotar
Observatory, California InstiMe
of Technology, Pasadena,
Abstract Time sequences of vector magnetograms Solar Observatories have provided us the opportunity
of Hauirou to identify
CA 91125
and Big Bear the individual
magnetic loops and athe separatrices between them. Based on the continuous observatin of vector magnetic field of NOAA 7469 from 4 to 12 April 1993, for the first time, the authors have identified the magnetic loop systems and relevant separatrices for such an active region. The observational signature ofthe cross-section of separatrices on the photosphere is as follows: (1) High degree of magnetic
shear at or close to the separatrices;
(2) Steep gradient of line-of-sight magnetic field (- 0.1 G/km) crossing neutral line. (3) Flux cancellation from both sides of the separatrices. At this point transverse field partly changes its alignment. During the observed period, flare activity of the separatrices. Key words:
solar active
region-vector
took place repeatedly
magnetic
the the
in the vicinity
field-flare
1. INTRODUCTION The role of the topology release of magnetic Since the 22nd accumulated a rich has reached a stage regions is possible. t Supported Received
of magnetic
field in determining
the evolution
of the field and the
energy has been increasingly appreciated by solar astrophysicists. solar cycle, Huairou Solar Observing Station, Beijing Observatory has set of data of vector magnetic field. Systematic observation of vector field where identification of topological features of the magnetic field of active The joint observation of the vector field by Huairou Station and Big Bear
by National Natural Science Foundation 1994-01-22; revised version 1994-0524
470
SHI Zong-xian et al.
Solar Observatory
has proved the reliability
of the measurement
of the transverse
field using
video-frequency magnetographs. Analysis of the data of the joint observation has convinced us, for the first time, that the analysis of the main loop systems and the variations in their interacting interface will provide process of flares itself. In an early
study
a new observational
of 6 sunspots,
Professor
Zirinl’l
basis for investigating pointed
out that
the physical
the two parts
of
opposite polarities of a 6 spot come from different sunspot pairs, and that at the separatrix, the field is highly sheared. Machado et al.121, basing on SMM X-ray imaging observation and vector magnetograms of Marshall Space Flight Center, were the first to propose that the interaction between two or more magnetic loops is the basic configuration for producing flares. But the magnetograms available to those authors did not have sufficient temporal and spatial resolutions for sure identification of loop systems and also lacked continuous observation over any prolonged period. examination of SHI and WANG13y41 using data of Huairou Station, made a systematic X-Class flares of the 22nd cycle before 1992 and found that 96% of the flares are connected with sunspot groups containing 5 spots during the lifetime of the active region, and found the magnetic flux ratio between the two polarities of the relevant 6 spot to be as large as 6.6 : 1. These findings further corroborated Zirin’s conclusion that the neutral line that goes across a 6 spot is located on a topological boundary. From theory, DCmoulin and Mandrini15-“1 using a simplified quadrupole model, simulated the field topology of active regions and demonstrated the extreme importance of magnetic topology in the energetic process of flares. In view of this, this paper attempts a further analysis of the magnetic field topology of active regions by using the vector magnetograms of Huairou Station and Big Bear Solar Observatory, in particular, we shall attempt to identify from the data, individual loop systems and the separatrices between them, and analyse the relation in space between the separatrices and flares, thereby hopefully gaining some new understanding on the flare process.
2. VECTOR
MAGNETOGRAMS
OF
ACTIVE
REGIONS
The vector magnetograms of Huairou Station are digitized magnetic maps. The longitudinal field is expressed by isogauss contours, the solid and dashed lines representing posFrom outside inwards, the contour values are itive and negative polarities, respectively. on the longituf20,40,80,160,320,640,960,1280, *. . G. The transverse field is superposed dinal field map, expressed by orientated line segments of different lengths (proportional to the filed). The transverse field has a 180° ambiguity. The magnetic maps of Big Bear Solar Observatory are essentially the same as the maps of Huairou Station. In the grey-scale maps, white means positive, black, negative polarity. The transverse field is expressed by superposed, equal line segments. Fig. 1 is the vector magnetogram of NOAA 7469. Fig. 2 is the vector magnetogram of Big Bear Observatory. NOAA 7470 enters the filed of view on April 8. North on top, West on right. All the features mentioned in the text, that is, the identified foot-points in the longitudinal field map, are labelled by a capital letter, e.g., D, H, M, etc.. All surely identified
471
Magnetic Separatrices
separatrices
are denoted
by joining
the two letters
of the foot-points
DZ, MH, etc.. From Figs. 1 and 2, we can see the course of evolution grey-scale
picture,
the active region
we can see fine field structure and its surrounding
3. IDENTIFICATION
network
on the two sides, e.g.,
of NOAA 7469. Particularly,
and evolution
of the interaction
in the between
field.
OF MAGNETIC
LOOPS
AND
SEPARATRICES
Magnetic loops and topological three-dimensional space. With
boundaries between them are structures and surfaces in the vector magnetograms we are only examining these features in the section of the photosphere (the Z - 0 section). See Ref. [9], Fig. 2. Hence, sometimes boundary surfaces (separatrices) become coincident with boundary lines (separators). Whether or not a given pair of positive and negative magnetic foot-points belong to
the same magnetic loop can be decided of the transverse field. If the transverse
by the continuity or otherwise of the orientation field between the two foot-points keeps the same
connections, then we can regard the two foot-points and the transverse field in between to represent the same magnetic loop. If the loop satisfies the condition offorce-free field, then its properties can be approximately described by one force-free parameter cr (“approximately”, because strictly speaking, IY varies from point to point within the loop). In this case, at the point where it crosses a boundary line in the longitudinal field (&I = 0), the transverse field does not change suddenly its direction, but rather continues with the original general direction , as at the locations marked 1 and 3 in the 6d2319(UT) map of Fig. 1. Around a boundary between two different loops, such continuity of transverse is not preserved and, rather, strong shear often appears. See the spaces between D and Z, and between M and H. So, these pairs of foot-points belong to different loops. An obliquely placed “S” is used to indicate strong shear. Continuous video recording shows the gradual diminishing of the positive foot-point D through cancellation with B and the decay of magnetic flux. By 8d0357(UT), only a vestige remains. Similarly, cancellation took place between C and H, the negative H gradually diminishing, while the orientation logical connectivity).
of the transverse
also changed
(implying
a changing
topo-
Additional evidence comes from changes in the longitudinal field gradient. For the two foot-points of the same loop, the distance between the opposite polarities of the longitudinal field increases in time, while those of different loops do the opposite. The field gradient evolves in opposite directions in the two cases. When the gradient reaches 0.1 G/km, magnetic cancellation will take place, that is, “slow” reconnection will start (the time scale of “slow” reconnection is one to two orders of magnitude longer than “fast” reconnection relevant to flares). The same sort of thing should happen at the boundaries between two active regions or between an active region and the network structure of the quiet region, but because of the weakness of the transverse field, shearing is often difficult to make out. In such cases, video recording or more frequency magnetic observations are necessary. A simultaneous decay of the longitudinal field gradient and both polarities would be an effective indicator. For example, on the boundary between active regions 7469 and 7470, at 8d1630(UT), features
472
SHI Zong-xian
Fig. 1 Evolution
et al.
of NOAA 7469 in the 4-day period 1993 April 6-10
Magnetic Separatrices
473
474
SHI Zong-xian
et al.
4
a
Magnetic Separatrices
475
Fig. 4 Showing the close relationship between the positions of flares (middle and bottom panels) and separatrices
DZ, CH and MH (top) on April 7
476
SHI Zong-xian et al.
Fig. 5 Showing the close relationship between the positions of flares (right) and separatrices CH, BJ and MH and the boundary between AR7469
and AR7470
(left) on April 8.
Fig. 6 Showing the close relationship between the positions of flares (right) and the boundary between AR 7469 and AR 7470 (left) on April 9
Magnetic Separatrices
Table
1
Relationship between Flares listed in S.G.D. and Separatrices
NO 1
Date 4.6
2
Time
--
184836
Lat
Opt/x-ray
CMD
--
07
12
DB,DZ DB,DZ
12
04
lB/M1.5
0507
12
01
SN
5
0613
11
00
SF/Cl.4
6 : I
0804
10
WOE
4.7
DZ,surge
SF
235650
4
Remarks
SFlC4.4
E08
s12
231814
3
477
DZ PG DZ
SF/Cl.3
PG DZ CH,BJ,MH
0214
13
10
SF
8
154452
11
19
SF
9
155408
06
18
SFlB9.9
7470,QR
10
193022
II
21
SF/Cl.5
CH,BJ,MH CH,BJ,MH
4.8
11
193656
11
21
SFjC6.5
‘12
221650
06
23
SF
7470,QR
13
223726
08
22
SF
7470,QR 7470,QR
162419
10
44
SF
15
201752
05
35
SF/Cl.2
7470,QR
16
231306
!6
40
lF
Bright
17
232352
I6
40
SF
CH,MH
14
4.9
surge,CH,MH
174323
06
$8
lN/C6.8
7470,QR
19
232327
07
54
SF/Cl.4
Bright
surge,CXI,MH
20
232400
08
51
1N/C9.1
Bright
surge,CH,MH
003656
12
53
lNlC6.2
Bright
surge,CH,MH
18
21
4.10
4.11
-
-
Figs. 3-6 illustrate the close relationship four days, April 6-9.
E, I, J and G all belong active regionsIi71.
4. LOCATIONS
to the network
between
structure
OF FLARES
the Ho flares and the separatrices
and they reconnected
RELATIVE
TO
on the
with the field of the
TOPOLOGICAL
BOUNDARIES
We use photographs of the TV screen to compare the positions of the flares and the boundaries. The images may not be very clear because of the limited resolution of the TV camera. Generally they give only the foot-points of the magnetograms and the Ha flares, the latter identified by sudden brightening in the Ha video recording. During the four days, April 6-9, there were 47 main Ha brightenings, all taking place around the topological boundaries between the magnetic loops. 11 occurred around DB or DZ, 15 around CH or MH. 10 between active regions 7469 and 7470. Of the rest, 5 were related to EA or IA, 6 to BJ, and 2 to PG. Table 1 lists the 21 flares published in S.G.D.I*‘l, together with the related boundaries and accompanying phenomena.
SHI Zong-xian et al.
478
5. DISCUSSION
5.1 In the vector magnetic field, whenever the transverse field crosses the polarity boundary of the longitudinal field (B 11 = 0) more or less perpendicularly, the two footpoints on either side of the boundary belong to the same magnetic loop. That is, there is no place where B = 0. By contrast, the magnetic boundary between different loops is a B = 0 curve (separator) in the three-dimensional spacelg~121. High resolution vector field observations
have shown
that
in places
of strong
shear,
we have not only
Blr
= 0,
but BI (the transverse field) is also nearly zero, hence such places are also locations of topological boundaries. When two magnetic loops interact, there is magnetic flux crossing the B = 0 surface, changing the old topology into a new one. And when this happens, we could say that, essentially, and speed of magnetic energy
magnetic reconnection has begun. Depending on the size release, various classes of flare will occur, accompanied by
mass ejection. Observations have also confirmed that frequency flares appear around the topological boundaries. Thus, the importance of interaction between different topological units on flare eruptions can be readily appreciated. 5.2 The phenomenon of magnetic cancellation is always connected with topological boundaries, and not with single magnetic loops. When magnetic reconnection takes place in the photosphere-the lower layer of the solar atmosphere, it is a sort of slow reconnection, its time scale is l-2 orders of magnitude longer than the fast reconnection. After heating the corona for some time, the slow reconnection eventually develops into a fast reconnection, although we are not clear about the conditions for the conversion. And fast reconnection means the start of flare110~‘71. 5.3 As long as the field configurations on either side of the boundary remain basically the same, magnetic reconnection will continue to take place, hence persistent flare activity on either side. As given in Table 1, flares were repeatedly observed around the boundaries DZ and DB, and CH and MH. Sometimes, a small happening on the boundary will give rise to a large event, for example, a small magnetic cancellation in NOAA 5572 caused an unwinding of the dark filamentsl’31. 5.4 The single loop model of the available theory of flares will have difficulty in explaining the results found here. As a matter of fact, in all the vector field observations so far, there has never been a confirmed
case of flares relating
This may be due to insufficient
resolution
to a single,
of magnetic
isolated
field telescopes
magnetic
10opl’~~‘~l.
and there should
be
further study on this question. 5.5 Vector magnetic field observation has now provided the possibility of identifying observationally active magnetic loops and topological boundaries, thereby raising flare observation and analysis to a new level. Perhaps it has provided a new clue to physical prediction .of flares. In 1992, Shi and Wang Us1 put forward the concept of “magnetic weather”, comparing the topological boundaries to the fronts in terrestrial weather, where frequent activities occur. 5.6 To conclude, continuous observation of vector magnetic field provides a new means of identifying magnetic loops and topological boundaries. The signature of a boundary is given in the Abstract. All the main flare activity happens in the vicinity of the boundaries. ACKNOWLEDGMENT
We have received
great
help from Beijing
Observatory,
Huairou
Magnetic
Station.
Professor
Zirin has provided
479
Separatrices
us with all the video tapes for analysing
the active
region.
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