A study of magnetic avalanches in Perminvar, an Fe-Ni-Co alloy, shows
that some avalanches are almost exactly reproducible from one magnetic
field cycle to the next, while others show significant variability. A
veraging over many cycles produces a fingerprint reflecting the reprod
ucibility of the noise. The fingerprint is not strongly temperature or
driving-rate dependent, indicating that the variability is a conseque
nce of dynamical effects. We also find that the slope of the cycle-ave
raged magnetization, d[M]/dH, is correlated with the cycle-to-cycle va
riations in magnetization, [(delta M)(2)].