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.