Interdecadal variability in the tropical Indian Ocean has been analyzed bas
ed on the long-term climatic observational data. Case study showed that str
ong interannual signals formed at the surface can penetrate the depth of se
asonal thermocline, where the anomalies last a couple of years. Artificial
time series based on damping with exponential decay of selected strong even
ts agree well with the detected interdecadal variability in the tropical In
dian Ocean. A possible dynamic explanation for interdecadal variability in
the tropical Indian Ocean was proposed that irregular interannual signals c
an lead to a slowly evolving climatic background with the interdecadal time
scale through damping of the memory about anomalies in the seasonal thermo
cline.