The variability of sea surface temperature (SST) in the tropical Atlan
tic Ocean has a significant influence on the rainfall over Northeast B
razil and the Sahel. The predictability of the SST fluctuations in thi
s region has, therefore, been a central concern for Atlantic climate s
tudies. Here we show that the north tropical Atlantic SST variability
has significant predictability using statistical models at short lead
times (less than or equal to 1 year), and using a coupled ocean-atmosp
here model for longer-range forecasts (lead times up to about 3 years)
, While the remote influence of the IndoPacific, primarily due to El N
ino, has been found to enhance the predictability of SST in the north
Atlantic at short lead times, local ocean-atmosphere interactions domi
nate the predictable dynamics farther south, and at longer time scales
.