NOAA 9077 is at the central meridian on 14 July. HSOS observed this active
region and obtained vector magnetic field data during good seeing conditions.
We choose 18 magnetograms (13-15 July, listed in Table 1) for the study of the
-configuration P6-F4. Because the active region is very close to
the disk center, we assume that the longitudinal field B|| can be
approximated by Bz. In the data reduction, we avoid the negative effects
listed in Sect. 2 for the reasons stated there. The vertical current
density is calculated by
![]() |
(1) |
We define the density of vertical current helicity as
![]() |
(2) |
Figure 6 shows the evolution of the current density for P6-F4 over three
days. The positive polarity of the magnetic field is given in white, while the
negative is given in black. Solid contours represent upward components of
current density, while dashed represent downward components. The levels of
current density are 2, 8, and 20 Am-2. Positions of P6 and F4 are
also precisely marked in this figure.
We find an obvious current reversing process for F4. On 13 July, F4 is
dominated by a large, positive current patch (its helicity is negative and the
same as the predominant, left-handed twist of the northern hemisphere). On 14
July, the current density of F4 is decreased and the patch separates from its
environment. Finally, its current density becomes negative on 15 July. During
the three days, the current of P6 retains the same negative polarity. From
Eq. (2) we can see that if the sign of the average vertical current is
reversed then the sign of the chirality (current helicity) will also be
reversed. We also demonstrate the process of helicity evolution in Table 1 and
Fig. 7. In Fig. 7, F4 and P6 are shown in the top two panels, the total
active region and the -configuration of F4-P6 are shown in the bottom
two panels. The helicity density of NOAA 9077 varies over a small range from
-2 to
G2 m-1, while the other three objects (F4,
P6, and F4-P6) fluctuate over wider ranges from near zero to more than
G2 m-1. At 05:53 UT on 14 July, F4 reverses
the helicity sign once (see Table 1), but returns to its original state in the
next magnetogram. This may be due to the onset of strong disturbance.
Between 08:12 UT and 08:43 UT, about two hours before the major flare, F4
alters irreversibly its chirality.
Copyright ESO 2002