Analyses of annual mean sea surface temperatures (SST) from observations fo
r the period 1903-94 and four different general circulation models (GCMs) w
ere conducted. The two dominant EOFs of all datasets are characterized by t
wo patterns, which are centered in the trade wind zones, at roughly 15 degr
ees N and 15 degrees S, respectively. The two patterns are uncorrelated at
any lag and the time spectra of the corresponding principle components are
consistent with red noise. The SST variability is strongly correlated with
wind stress anomalies in the trade wind zones. The correlations between the
wind stress and the SST, as well as the correlation between the net heat f
lux and the SST anomalies are consistent with the assumption that the varia
bility of the upper tropical Atlantic Ocean is forced by the atmosphere. Dy
namic feedbacks of the tropical Atlantic Ocean are less important. The vari
ability in the trade wind zones shows a weak correlation with the ENSO mode
in the tropical Pacific.