Ion cyclotron emission (ICE) has been observed during D-T discharges i
n the Tokamak Fusion Test Reactor (TFTR), using RF probes located near
the top and the bottom of the vacuum vessel. Harmonics of the alpha c
yclotron frequency (Omega(alpha)) evaluated at the outer midplane plas
ma edge are observed at the onset of the beam injection phase of TFTR
supershots and persist for approximately 100-250 ms. These results are
in contrast with observations of ICE in JET, in which harmonics of Om
ega(alpha) evolve with the alpha population in the plasma edge. Such d
ifferences are believed to be due to the fact that newly born fusion a
lpha particles are super-Alfvenic near the edge of JET plasmas, while
they are sub-Alfvenic near the edge of TFTR supershot plasmas. In TFTR
discharges with edge densities such that newly born alpha particles a
re super-Alfvenic, alpha cyclotron harmonics are observed to persist.
These results are in qualitative agreement with numerical calculations
of growth rates due to the magnetoacoustic cyclotron instability.