GEOPHYSICAL MONOGRAPH SERIES, VOL. 147, PP. 121-142, 2004
Tropical Atlantic variability: Patterns, mechanisms, and impacts
International Pacific Research Center and Department of Meteorology, University of Hawaii, Honolulu, Hawaii
Department of Meteorology, University of Maryland, College Park, Maryland
This chapter reviews the progress made in the past decade in understanding tropical Atlantic climate variability. In addition
to an equatorially anti-symmetric seasonal cycle forced directly by the seasonal march of the sun, Atlantic sea surface temperature
(SST) displays a pronounced annual cycle on the equator that results from continental monsoon forcing and air-sea interaction.
This cycle interacts with and regulates the meridional excursions of the Atlantic intertropical convergence zone (ITCZ). On
interannual timescales, there is an equatorial mode of variability that is similar to El Niño/Southern Oscillation (ENSO)
in the Pacific. This Atlantic Niño is most pronounced in boreal summer coinciding with the seasonal development of the equatorial
cold tongue. In boreal winter, both ENSO and the North Atlantic Oscillation exert a strong influence on the northeast trades
and SST over the northern tropical Atlantic. In boreal spring when the equatorial Atlantic is uniformly warm, anomalies of
cross-equatorial SST gradient and the ITCZ are closely coupled, resulting in anomalous rainfall over northeastern Brazil.
There is evidence for a positive air-sea feedback through wind-induced surface evaporation that organizes off-equatorial SST
anomalies to maximize their cross-equatorial gradient. The resultant anomalous shift of the ITCZ may affect the North Atlantic
Oscillation, helping to organize ocean-atmospheric anomalies into a pan-Atlantic pattern.
Citation: Xie, S.-P., and