Some 5 per cent of bright meteors show rapid, quasi-periodic brightness var
iations. It is argued that this effect, observationally known as flickering
, is a manifestation of the rotational arg modulation of surface mass loss
through ablation of a non-spherical meteoroid. We develop a set of time-dep
endent, single-body ablation equations that include the effect of cross-sec
tion area modulation. We present a discussion of the effects that the rotat
ion of a non-spherical meteoroid has on the resultant meteor light curve, a
nd we took in depth at the data related to the fireball associated with the
fall of the Innisfree meteorite. We find that the parent object to the Inn
isfree meteorite was spinning at a rotation frequency of 2.5 Hz when it enc
ountered the Earth's upper atmosphere. We also find that the Innisfree pare
nt body had an initial mass of about 20 kg and that the ratio of its semimi
nor and semimajor axes was about 0.5.