PRECIPITATION (rain and snow) provides, through its participation in t
he global hydrological and energy cycles, most of the heat flux within
the atmosphere, For this reason, a knowledge of precipitation variabi
lity is important to understanding the behaviour and changes of the Ea
rth's climate system, Precipitation measurements have been made at tho
usands of sites over the past hundred years or so, and recent efforts
have resulted in the compilation of global data sets(1-3) and regional
networks(4,17) . The latter have been analysed to reveal high-frequen
cy (up to interannual) regional trends in precipitation variability ov
er the past century(4). Here I exploit the global data sets to examine
the low-frequency (decadal to multi-decadal) variability of precipita
tion over a similar time period, In agreement with other analyses(5),
I find that the global mean precipitation has not changed. The fluctua
tions about the mean, however, have increased significantly (on decada
l to multi-decadal timescales), That is, over the past century-during
which climate warming has occurred-the global precipitation field has
undergone changes on those scales, in which extremes have become more
probable, This result is consistent with predictions from model simula
tions of global climate-warming scenarios(6-8).