A study of solar wind acceleration based on gyrotropic transport equations

Authors
Citation
El. Olsen et E. Leer, A study of solar wind acceleration based on gyrotropic transport equations, J GEO R-S P, 104(A5), 1999, pp. 9963-9973
Citations number
36
Categorie Soggetti
Space Sciences
Journal title
JOURNAL OF GEOPHYSICAL RESEARCH-SPACE PHYSICS
ISSN journal
21699380 → ACNP
Volume
104
Issue
A5
Year of publication
1999
Pages
9963 - 9973
Database
ISI
SICI code
0148-0227(19990501)104:A5<9963:ASOSWA>2.0.ZU;2-H
Abstract
The gyrotropic transport equations are used to describe an electron-proton solar wind from the 500,000 K level in the upper transition region and out to 30 solar radii. These equations allow for different temperatures paralle l and perpendicular to the magnetic field, as well as transport of parallel and perpendicular thermal energy along the field. We find that in models w ith significant coronal proton heating, the electron temperature is much lo wer than the proton temperature. The electron gas is collision dominated, t he thermal anisotropy is small, and the heat flux is close to a "classical" heat flux. The proton gas is collision dominated in the upper transition r egion, but the temperature increases rapidly in the inner corona, and the p rotons become collisionless close to the Sun. The proton heat flux is propo rtional to the temperature gradient very close to the Sun, but in the exten ded corona it deviates substantially from a classical heat flux. In models where the proton heating is in the direction perpendicular to the magnetic field, a large perpendicular temperature is produced locally, but the perpe ndicular thermal motion couples into parallel thermal motion, and the paral lel temperature increases outward from the Sun. We obtain a maximum paralle l temperature that is comparable to the maximum perpendicular temperature. This result seems to hold for all models where the energy flux necessary to drive high-speed wind is deposited in the corona as heat. The result is no t in agreement with UVCS/SOHO observations of the 1216 Angstrom Ly-alpha li ne in large coronal holes. These observations are consistent with a much la rger random proton motion perpendicular to the magnetic field than parallel to the field. Such anisotropies can be obtained in models of high-speed so lar wind if we allow for a significant fraction of the energy flux from the Sun to be in the form of low-frequency, transverse waves. These waves acce lerate the solar wind without heating the corona, and they contribute to th e line broadening in the direction perpendicular to the magnetic field.