A large increase in electron temperature measured in filamentary aurora wit
h the European incoherent scatter radar has been modeled with a one-dimensi
onal electron transport and ion chemistry code. To account for the observed
changes in electron temperature, while also reproducing the measured E reg
ion electron density profiles, a source of electron heating is required in
addition to local heating from energy degradation of the precipitating elec
trons. We show that ohmic heating in a strong field-aligned current can acc
ount for the required heat source.