The recognition of natural modes of climate variability is essential f
or a better understanding of the factors that govern climate change. R
ecent models suggest that interdecadal (roughly 15-35-year period)(1-4
) and century-scale (roughly 50-150-year period)(5-7) climate variabil
ity may be intrinsic to the natural climate system. While there is som
e evidence for the existence of interdecadal(8,9) and century-scale(9,
10) oscillations in instrumental temperature records, confident detect
ion from these short (100-400-year) records is difficult(11,12). Oscil
lations on the same timescales(5,13-17) have also been detected in iso
lated climate-proxy or historical records over longer durations, but t
he large-scale spatial structure of the variability has not been inves
tigated systematically. Here we report the multivariate analysis of a
globally distributed set of temperature proxy records of several centu
ries duration. The results of our spatio-temporal analysis strengthen
evidence for persistent natural interdecadal and century-scale climate
oscillations, and reveal both the spatial patterns and temporal histo
ries of these signals.