The Angola-Benguela Front is the generic border between, on the one hand, t
he Benguela Current and the coastal upwelling regime along the southwest Af
rican coastline and, on the other hand, the warm, southward flowing Angola
Current. This frontal zone has a variable morphology, geographic location,
and thermal characteristics. It has been suggested that this variability ma
y be related to changing wind patterns. We have studied the thermal charact
eristics of the surface expression of the frontal zone for a 74-day period
using daily thermal infrared images and compared-these to wind patterns fro
m synoptic weather maps. There is little correlation between the location o
f the northern and the southern front that form the envelope for this front
al zone. The location of the southern front largely determines the thermal
gradient across the entire frontal zone. Large short-term displacements in
the geographic location of the frontal zone as well as short-term variation
s in its thermal characteristics are shown to be strongly correlated to the
atmospheric pressure gradient of the South Atlantic anticyclone with a 1-d
ay lag period. This is true irrespective of the latitude changes of the cen
ter of the South Atlantic anticyclone.