An analysis of historical sea surface temperatures provides evidence f
or global warming since 1900, in line with land-based analyses of glob
al temperature trends, and also shows that over the same period, the e
astern equatorial Pacific cooled and the zonal sea surface temperature
gradient strengthened. Recent theoretical studies have predicted such
a pattern as a response of the coupled ocean-atmosphere system to an
exogenous heating of the tropical atmosphere. This pattern, however, i
s not reproduced by the complex ocean-atmosphere circulation models cu
rrently used to simulate the climatic response to increased greenhouse
gases. Its presence is likely to lessen the mean 20th-century global
temperature change in model simulations.