A method of separating the contributions from slowly varying boundary forci
ng and internal dynamics (e.g. intraseasonal oscillations) that determine t
he predictability of the monthly mean tropical climate is presented. Based
on 33 years of daily low level wind observations and 24 years of satellite
observations of outgoing long wave radiation, we shoes that the Indian mons
oon climate is only marginally predictable, as the contribution of the boun
dary forcing in this region is relatively low and that of the internal dyna
mics is relatively large. Pt is also shown that excluding the Indian monsoo
n region, the predictable region is larger and predictability is higher in
the tropics during northern summer. Even though the boundary forced varianc
e is large during northern winter, the predictable region is smaller as the
internal variance is larger and covers a larger region during that period
(due to stronger intraseasonal activity).