Dispersive effects in field line resonances (FLRs) are discussed in the con
text of potential structures, parallel currents, and auroral density caviti
es observed by the FAST satellite. Our model includes the Earth's dipole ma
gnetic field, and accounts for electron inertia, electron thermal pressure,
finite ion gyroradius effects, and field aligned variations of the plasma
density and ambient electron and ion temperatures. For realistic backgound
parameters, we show that finite plasma temperature effects determine the dy
namics of FLRs and that solitary wave structures evolve out of the resonanc
e region, producing deep density cavities above the polar ionospheres. Resu
lts are shown to be in reasonable agreement with ground and satellite obser
vations, with the exception of the magnitude of low altitude electric field
s.