The combination of high time and space resolution measurements in the
magnetic zenith (optical and radar) and detailed modeling of the ionos
pheric response to auroral particle precipitation has produced the new
result that most of the energy density in a bright are resides in an
extremely narrow filament, embedded in a broader feature. We are able
to show that the narrow filaments, of the order of 100 m width, are pr
oduced by monoenergetic beams of electrons, whereas the surrounding em
issions of lower energy density are produced by broad spectral distrib
utions. The new result is achieved by combining different energy spect
ra as input to an auroral model and comparing the resulting electron d
ensity profiles with those measured with the European incoherent scatt
er radar at 0.2 s time resolution. The result is dependent on the opti
cal evidence that the narrow energetic beams do not fill the fields of
view of the detectors, i.e. both photometer and radar. Agreement betw
een the observed structure, scale lengths, and evolution of the aurora
and modeled predictions suggests that transient parallel electric fie
lds are important acceleration mechanisms above the ionosphere.