Solar wind frequency spectra show a distinct steepening of the f(-5/3)
power law inertial range spectrum at frequencies above the Doppler-sh
ifted ion cyclotron frequency. This is commonly attributed to dissipat
ion due to wave-particle interactions. We consider the extent to which
this steepening can be described, using a magnetohydrodynamic formula
tion that includes the Hall term. An important characteristic of Hall
MHD is that although the ion cyclotron resonance is included, there is
no wave-particle dissipation of energy. In this study we use a compre
ssible Hall MHD code with a constant magnetic field and a polytropic e
quation of state. Artificial dissipation in the form of a bi-laplacian
operator is used to suppress numerical instabilities, allowing for a
clear separation of the dissipative scales from the ion cyclotron scal
es. A distinct steepening appears in the simulation power spectra near
the cyclotron resonance for certain types of initial conditions. This
steepening is associated with the appearance of right circularly pola
rized fluctuations at frequencies above the ion cyclotron resonance. S
imilar steepenings and polarization enhancements are observed in solar
wind magnetic held data.