Earlier model studies of solar wind driven by thermal pressure and Alf
ven waves have shown that wave amplitudes of 20-30 km s-1 at the coron
al base are sufficient to accelerate the flow to the high speeds obser
ved in quasi-steady streams emanating from large coronal holes. In thi
s paper we focus on the energy balance in the proton gas and show that
heat conduction from the region where the waves are dissipated may pl
ay an important role in determining the proton temperature at the orbi
t of Earth. In models with ''classical'' heat conduction we find a cor
relation between high flow speed, high proton temperature, and low ele
ctron temperature at 1 AU. The effect of wave heating on the developme
nt of anisotropies in the solar wind proton gas pressure is also inves
tigated in this study.