Ion Temperatures in a Solar Polar Coronal Hole Observed by Sumer onSOHO
Open Access
- 10 August 1998
- journal article
- research article
- Published by American Astronomical Society in The Astrophysical Journal
- Vol. 503 (1) , 475-482
- https://doi.org/10.1086/305982
Abstract
The temperatures of some highly charged ions in the southern solar polar coronal hole are determined from the widths of the extreme ultraviolet (EUV) lines measured by the SUMER (Solar Ultraviolet Measurements of Emitted Radiation) instrument on SOHO (Solar and Heliospheric Observatory). Radiation from both light ions, such as Ne6+, Ne7+, Mg7+, Mg9+, Si6+, and Si7+, and heavy ions, such as Fe9+, Fe10+, and Fe11+, are recorded in off-limb observations. We refer here to the limb as the height, h0, where the limb brightening of the N IV 765 Å line maximizes. After correction of the measured line widths for instrument contributions, the intrinsic widths of these emission lines are derived. These are produced by thermal motions of the ions and turbulent wave motions of the background plasma. Since the turbulent line broadening should be the same for all the different ions, its upper limit can be determined from the widths of the iron lines, assuming zero iron temperatures. Thus, the range of kinetic temperatures permitted for the light species can be delimited. For example, the average temperature of Ne7+, at heights above the southern limb relative to h0 from 17'' to 64'', ranges between 1.3 and 5 × 106 K, and the average temperature of Ne6+ ranges between 1 and 4 × 106 K. The interpretation of these measurements does not require knowledge of the ion formation (or electron) temperature. It is also found that the ion thermal speed decreases with increasing mass per charge, while the ion temperature remains roughly constant. In another observation at heights from 167'' to 183'' above h0, the temperature of the ions increases slightly with increasing mass per charge, while the thermal speed reveals no clear trend. The upper limits of the turbulence amplitude, δv21/2, derived for these two altitude ranges are 33-37 and 44 km s-1, respectively. The implications of these results for the heating of the solar corona and the acceleration of the solar wind are discussed.Keywords
This publication has 21 references indexed in Scilit:
- The fast solar windGeophysical Research Letters, 1997
- A Coronal Spectrum in the 500–1610 A Wavelength Range Recorded at a Height of 21,000 Kilometers above the West Solar Limb by the SUMER Instrument on Solar and Heliospheric ObservatoryThe Astrophysical Journal Supplement Series, 1997
- Electron Density Diagnostics for the Solar Upper Atmosphere from Spectra Obtained by SUMER/SOHOThe Astrophysical Journal, 1997
- Electron Densities in the Solar Polar Coronal Holes from Density-Sensitive Line Ratios of [CLC]Si[/CLC] [CSC]viii[/CSC][CLC]and S [CSC]x[/CSC] [CLC][/CLC][/CLC]The Astrophysical Journal, 1997
- Determination of the Formation Temperature of [CLC]Si[/CLC] [CSC]iv[/CSC] in the Solar Transition RegionThe Astrophysical Journal, 1997
- FIRST RESULTS OF THE SUMER TELESCOPE AND SPECTROMETER ON SOHO – II. Imagery and Data ManagementSolar Physics, 1997
- A burst model for line emission in the solar atmosphere. III - A reassessment of the assumptions of constant pressure and steady state coronal equilibrium in the solar transition regionThe Astrophysical Journal, 1993
- ON THE POSSIBLE ROLE OF PLASMA WAVES IN THE HEATING OF CHROMOSPHERE AND CORONAPublished by Elsevier ,1992
- THE ORIGIN OF HIGH SPEED SOLAR WIND STREAMSPublished by Elsevier ,1992
- Line broadening of MG X 609 and 625 A coronal emission lines observed above the solar limbThe Astrophysical Journal, 1990