This lecture discusses the low-frequency variability of surface temperature
using a coupled ocean-atmosphere-land-surface model developed at the Geoph
ysical Fluid Dynamics Laboratory/NOAA, Despite the highly. idealized parame
trization of various physical processes, the coupled model simulates reason
ably well the variability of local and global mean surface temperature. The
first half of the lecture explores the basic physical mechanisms responsib
le for the variability. The second half examines the trends of local surfac
e temperature during the last half century in the context of decadal variab
ility simulated by the coupled model.