DIRECT AND INVERSE CASCADES IN THE ACCELERATION REGION OF THE FAST SOLAR WIND

Alfven waves are believed to play an important role in the heating and acceleration of the fast solar wind emanating from coronal holes. Nonlinear interactions between the dominant z(+) waves and minority z(-) waves have the potential to transfer wave energy either to smaller perpendicular scales ("direct cascade") or to larger scales ("inverse cascade"). In this paper we use reduced magnetohydrodynamic (RMHD) simulations to investigate how the cascade rates.. depend on perpendicular wavenumber and radial distance from the. Sun center. For models with a smooth background atmosphere, we find that an inverse cascade (is an element of(+) < 0) occurs for the dominant waves at radii between 1.4 and 2.5 R. and dimensionless wavenumbers in the inertial range (15 < a(perpendicular to) < 44), and a direct cascade (is an element of(+) > 0) occurs elsewhere. For a model with density fluctuations, there are multiple regions with an inverse cascade. In both cases, the cascade rate is an element of(+) varies significantly with perpendicular wavenumber, indicating that the cacsade is a highly nonlocal process. As a result of the inverse cascades, the energy dissipation rates are much lower than expected from a phenomenological model. and are insufficient to maintain the temperature of the background atmosphere. We conclude that RMHD models are unable to reproduce the observed properties of the fast solar wind.