The wavelet transform is applied to the analysis of active region oscillati
ons. The localised (in time) nature of the wavelet transform allows us to s
tudy both the duration of any statistically significant oscillations as wel
l as their period. Time series arising from SOHO (Solar and Heliospheric Ob
servatory) CDS-NIS (Coronal Diagnostic Spectrometer Normal Incidence Spectr
ometer) active region observations on 14th-15th November 1996 are used to d
emonstrate the applicability of wavelet methods. High cadence (approximatel
y 14 seconds) observations were made in He I 584.33 Angstrom (log T-e = 4.3
), O V 629.73 Angstrom (log T-e = 5.3), Mg IX 368.06 Angstrom (log T-e = 6.
0), Fe XVI 360.76 Angstrom (log T-e = 6.4) provide detailed intensity infor
mation on the active region over a wide range of temperatures. The distribu
tion of statistically significant periods found varies from line to line, a
s does their duration.