Astron. Astrophys. 364, 859-872 (2000)
1. Introduction
There has been much previous work on solar flares that has centered
around the understanding of the observed non-thermal broadening of
soft X-ray (SXR) emission lines. The non-thermal broadening is defined
as the difference between the Doppler temperature
( ) and the plasma temperature
( ). In an ionized He -like species
these temperatures are derived from the width of the main resonance
line and the ratio of the main resonance line and the satellite lines
respectively. This temperature difference is often expressed as a
non-thermal velocity ( ) where;
![[EQUATION]](img4.gif)
where k is the Boltzmann constant and
the mass of the ion under
consideration.
Studies of characteristics have
been carried out by a number of spaced based instruments, including
Skylab, P78-1 and the Solar Maximum Mission (SMM). Results from these
studies (e.g. Doschek et al. 1986) showed that they can be
approximated as Gaussian broadening with peak values ranging from
to .
They are present before the peak of the hard X-ray (HXR) flux and
diminish to between and
by the time of SXR maximum. There is
no correlation observed between maximum
and position on the disk. There is
also evidence for the presence of in
CIV ( ) spectral lines
at .
In a large study of small flares Harra-Murnion et al. (1997)
examined the variation of with
electron temperature, GOES classification, duration of event, rise
time and source size of the SXR event. Their results showed that
is independent of flare size,
complexity and intensity of hard X-ray (HXR) bursts, but there is a
weak dependence on duration and rise time. The longer the rise time
the lower the value of and there is a
trend of increasing with ele ctron
temperature.
However, the nature and location of the source of the non-thermal
broadenings is still unknown as indeed is its role in the flare
process. For example, are they a direct signature of the flare energy
release process, or a hydrodynamic response of the solar atmosphere to
the injection of flare energy? Fig. 1 shows a schematic diagram
of a proposed unified flare model (Shibata 1999). Within this single
loop flare model there exist five plausible locations where the source
of could be located. These five
regions are numbered on Fig. 1 and are described below.
-
1) The Reconnection Site: At the site of magnetic field line
reconnection and possible particle acceleration, the density must be
small to allow for efficient particle acceleration (Miller et al.
1997) and will have very small spatial scales. Thus the emission
measure is likely to be low. New evidence for the presence of inflows
to the reconnection region has recently been presented (Yokoyama
2000), however the reconnection region itself remains unresolved.
Hence this region is an unlikely source of the observed
.
-
2) The above the loop HXR source: The nature of the HXR above the
loop top source is still a topic of considerable debate (Fletcher
1999; Somov 1999). The two most popular explanations for the creation
of HXRs above the loops are from a super-hot source
( ) generated by the fast shock
(Masuda 1994; Tsuneta et al. 1997; Tsuneta & Naito 1998) or from
thin-thick target Bremsstrahlung from trapped electrons (Wheatland
& Melrose 1995; Fletcher & Martens 1998; Metcalf &
Alexander 1999). This above the loop source is believed to be confined
by two slow mode shocks that extend down from the reconnection region
(not shown in Fig. 1) and confine the energetic electrons by
acting as magnetic mirrors (Tsuneta & Naito 1998). Very hot SXR
plasma has also been observed to originate from above the loop top and
is believed to be heated by the slow shocks (Tsuneta 1996; Tsuneta et
al. 1997)
-
3) The SXR loop top: Unusually bright loop tops have been reported
by Doschek & Feldman (1996) using SXT, the presence of which can
be explained by the model of Jakimiec et al. (1998) which invokes a
turbulent loop-top kernel within which the magnetic field is tangled
and transient current sheets occur.
-
4) Evaporating chromospheric plasma: This is a direct consequence
of the flare electron deposition at the footpoints, initiated when the
energy deposition rate greatly exceeds the rate at which the energy
can be conducted and radiated away. The plasma expands explosively and
is driven up the magnetic loop into the corona by strong induced
pressure gradients.
-
5) Flare loop footpoints: Visible at HXR, chromospheric and
transition region wavelengths, these result from the deposition of
flare electrons in the chromosphere at the base of the magnetic loop,
where they produce HXRs via thick target Bremsstrahlung and supply
heat to the chromosphere.
The regions described above are created by a variety of different
processes associated with a flare. By eliminating regions that are not
responsible for producing the observed non-thermal broadenings and
ultimately locating the region(s) of the flare that are responsible,
we can eliminate and identify possible mechanisms responsible for the
generation of .
In order to distinguish between these possibilities, studies of
occulted limb flares, in which the flare footpoints are obscured by
the solar disk, have been undertaken (Khan et al. 1995; Mariska et al.
1996; Mariska & McTiernan 1999). Khan et al. (1995) and Mariska
& McTiernan (1999) showed that for partially occulted limb flares
the measured was similar to that
observed for disk flares, indicating that the source of the
could not be the flare footpoints
since these were occulted by the limb. Khan et al. (1995) concluded
that the source of the was at the
loop top or that is the same
throughout the loop. These results are contradictory to those of
Mariska et al. (1996) who, using a smaller data set, showed a tendency
for occulted flares to have a lower
.
Doschek et al. (1986) and Mewe et al. (1985) have suggested that
the observed can be explained by the
fact that full Sun Bragg crystal spectrometers observe an integrated
spectrum of plasma moving at a range of velocities. Fludra et al.
(1989) showed a weak correlation between
and the measured blue shift velocity
and Mariska et al. (1993) showed a correlation between line width and
the line centroid shift. These results indicate that chromospheric
evaporation could account for at least some of the observed
particularly after the flare
impulsive phase.
Recent work by Ding et al. (1999) using 2D spectra of a resolved
flare loop has shown that the
profiles are more broadened at the loop top than anywhere else along
the loop. However, although the
loops are believed to cool from SXR loops, this result should not be
taken as true for SXR loops as well since flare loops in
H are often only seen when the SXR
non-thermal broadenings have decayed.
Knowledge of how the values of
develop over time can also place stringent criteria on the location
and generation of the . Alexander et
al. (1998) studied the relationship between the peak times in
and the HXR flux and showed that the
peak of the occurred before the
maximum in hard X-rays. Mariska & McTiernan (1999) in a similar
study of a larger sample observed that, for the majority of the events
they studied, the peak in occurs
after the first significant HXR peak, although the opposite behaviour
was seen in a minority of events. The attainment of high values of
early in a flare, a similar result
from both studies, is more indicative of plasma turbulence rather than
hydrodynamic flows as the source of
(Alexander et al. 1998).
The aim of this paper is to determine the location of the
non-thermal broadenings seen in the Yohkoh BCS
CaXIX channel. By determining the location of the
source of it will be possible to
eliminate some probable generation
mechanisms and possibly determine their role in the flare process. To
accomplish this goal we use multi-wavelength data from the SXT, BCS,
HXT instruments on Yohkoh in conjunction with TRACE. In
Sect. 2 we outline the instrumentation used in this study and in
Sect. 3 describe the basic properties of the studied flare. In
Sect. 4 we describe the method used to locate source of the
and present our results which
eliminate the footpoints as the source of
. In Sect. 5 we discuss the
implications of our results and probable locations for the source of
.
© European Southern Observatory (ESO) 2000
Online publication: January 29, 2001
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