The first test of a self-consistent theory for the combined electron-p
roton-hydrogen (H) atom aurora is presented. Specifically, the upgoing
differential electron flux that results from precipitating protons an
d electrons is modeled and compared to observations. The observations
are from the Low Altitude Plasma instrument (LAPI) on board the Dynami
cs Explorer 2 satellite. Excellent agreement between data and theory i
s produced when a kappa distribution is used to extrapolate the observ
ed proton spectra to energies beyond the instrument's energy cutoff (2
7 keV). More definitive tests of the model will require more comprehen
sive observations as well as improvements in available proton-H atom c
ross sections. However, it is concluded that data clearly supports the
theoretical prediction that the secondary electron spectra due to pre
cipitating protons and H atoms is much softer than that produced by pr
ecipitating electrons. Also, the implication that the incoming proton
spectra have a high-energy power law tail raises the possibility that
previous determinations of the total ion energy flux are too low.