Dynamic behavior of the upper solar atmosphere: SUMER/SOHO observations ofhydrogen Lyman lines

Citation
W. Curdt et P. Heinzel, Dynamic behavior of the upper solar atmosphere: SUMER/SOHO observations ofhydrogen Lyman lines, ASTROPHYS J, 503(1), 1998, pp. L95-L100
Citations number
12
Categorie Soggetti
Space Sciences
Journal title
ASTROPHYSICAL JOURNAL
ISSN journal
0004637X → ACNP
Volume
503
Issue
1
Year of publication
1998
Part
2
Pages
L95 - L100
Database
ISI
SICI code
0004-637X(19980810)503:1<L95:DBOTUS>2.0.ZU;2-W
Abstract
We present first observations of the temporal evolution of hydrogen Lyman l ines, made by the Solar Ultraviolet Measurements of Emitted Radiation (SUME R) spectrometer on the Solar and Heliospheric Observatory. A time series of about 33 minutes was obtained on 1997 June 5. The entrance slit has crosse d a quiet-Sun region of 115." 3 with two internetwork structures (cells) an d the bright network regions. A data set of 59 spectra with 30 s exposure t ime was obtained, using the SUMER tracking system to compensate for the sol ar rotation. For our analysis, we have selected a Lyman continuum window ar ound 907 Angstrom and the three Lyman lines Ly5, Ly9, and Ly15, which are f ormed at different depths in the upper chromosphere. In the cell interiors, we have detected significant periodic intensity variations with a Fourier transform power peak at 3.3-3.5 minutes, which is consistent with 3 minute internetwork oscillations. They seem to be associated with spatially unreso lved "clusters" of grains. In the bright network regions, we detect slower oscillations of 6.9-7.6 minutes. These waves seem to propagate upward as we deduce from a phase shift between the three Lyman lines studied. The phase velocity was estimated to be roughly 3 km s(-1) in the network. Finally, w e discuss the potential usefulness of the hydrogen Lyman lines for diagnost ics of the temperature structure of the upper solar atmosphere. Our observa tions, in particular the fact that we see all Lyman lines in emission all o f the time, put certain constraints on the temperature gradients above the region in which numerical simulations do predict a decrease of the mean kin etic temperature.