Inertial Alfven waves propagating in regions of auroral electron accelerati
on are observed from the FAST (Fast Auroral Snapshot) spacecraft over its e
ntire altitude range (350-4180 km). These electron skin depth sized field s
tructures are dispersive and carry an electric field component parallel to
the geomagnetic field leading to a variety of non-linear effects including
the formation of magnetic field-aligned density cavities and electron accel
eration. High resolution measurements show that the electron distribution i
nside the impulsive wave field envelope or density cavity consists of a col
d ionospheric component and an accelerated and heated field-aligned compone
nt comprised of downgoing and reflected ionospheric and magnetosheath (sola
r wind like) electrons. In large amplitude examples the plasma within the w
ave may be dominated by the accelerated component and the depletion of plas
ma within the cavity approaches 100%. Comparison of the observed density de
pletion with the predictions of ponderomotive density cavity Formation in a
ssociation with electron heating shows good agreement. Furthermore, simulat
ions show that most of the observed features of the accelerated component c
an be explained through Landau resonance of the cold ionospheric and magnet
osheath electrons with the inertial Alfven wave as it propagates through an
altitude dependent density profile.