Using the data for the period 1914-83, rainy and dry seasons of easter
n Northeast (ENE) Brazil are determined. The principal rainy season is
April through July (60% of the annual rainfall), and the principal dr
y season is September through December (10% of the annual rainfall). T
he fall and winter rains over ENE Brazil are associated with southeast
erly winds blowing perpendicular to the coast. The subtropical high in
the South Atlantic modulates the strength and direction of winds alon
g the coast that have a determining influence on the interannual varia
tions of rainfall over ENE Brazil. The possible link between the rainf
all over ENE Brazil and SST anomalies in the Atlantic is examined. The
SST anomalies of the season January, February, March, April (JFMA) in
the southeast Atlantic are positively correlated with the rainfall an
omalies of ENE Brazil. The sea surface temperature (SST) anomaly patte
rn frequently becomes established by January/February over southeast A
tlantic suggesting the predictive value of SST anomalies over southeas
t Atlantic for the rainfall over ENE Brazil.