The Far Ultraviolet Instrument (FUV) on the IMAGE spacecraft observes the a
urora in three different channels. One of them (SI12) is sensitive to the s
ignal from precipitating protons, while the other two (WIC and SI13) observ
e auroral emissions which are not only excited by precipitating electrons,
but also by protons. We examine a period when in-situ particle measurements
by the FAST spacecraft were available simultaneously with global imaging w
ith FUV. The measured electron and proton energy spectra are used to calcul
ate the auroral brightness along the FAST orbit. The comparison with the FU
V/IMAGE observations shows good quantitative agreement and demonstrates tha
t under certain circumstances high proton fluxes may produce significant am
ounts of auroral FUV emission.