 |  |
Astron. Astrophys. 351, 1139-1148 (1999)
1. Introduction
There are abundant references to solar electron density
(Ne) diagnostics in the literature, with e.g.
emission lines arising from transitions in O IV
providing accurate determinations of Ne (Griffiths
et al. 1999, Doschek et al. 1998, O'Shea et al. 1998, Spadaro et al.
1994, Dwivedi & Gupta 1991, Hayes & Shine 1987, Feldman &
Doschek 1978). For instance, Hayes & Shine (1987) used the ratio
of Si IV 1402.8 Å and
O IV 1401.2 Å, and found that
short-lived bursts typically showed electron density increases coupled
with a small line shift to the red. They suggested this might be
caused by ` micro-flares '. Cheng (1980), analysing coronal loops in
Fe XV & Fe XVI lines, found a
density enhancement of in a loop
within 7 minutes, plus a slower variation over a longer time interval.
He suggested that this increase in density could be due to mass
ejection from lower regions, and the associated dissipation of the
electric current associated with the resulting high-density twisted
flux strands (Nakagawa & Stenflo 1979) contributing to the coronal
heating.
In this paper we use the O IV
2 2p2
2s2p4P
density-sensitive multiplet around 1400 Å to analyse
time-series solar spectra. More precisely, we use the
O IV 1399.8 Å and 1401.2 Å
lines for our analysis.
The Solar Ultraviolet Measurements of Emitted Radiation (SUMER)
instrument (Wilhelm et al. 1997) on SOHO provides the
opportunity to observe the solar atmosphere in the spectral range from
500 to 1600 Å with high spectral
and spatial resolution. In first order, the spectral resolution is
43mÅ, while
22mÅ is achieved in second
order. The spatial resolution is approximately 1 arc sec in the E-W
direction and 2 arc sec along the slit (N-S direction). It should be
pointed out that only lines separated by less than 40 Å in first
order, and 20 Å in second order, can be observed simultaneously
with SUMER due to the size of the CCD. Surprisingly few lines can be
used for density diagnostics, due to blending problems, the weakness
of some lines, and the fact that possible useful lines cannot be
observed simultaneously. The line pair most useful for diagnosing the
transition region is probably O IV
1399.8 1401.2 (Wikstol et al.
1997).
© European Southern Observatory (ESO) 1999
Online publication: November 16, 1999
helpdesk.link@springer.de  |