Satellite observations of the Agulhas Current and episodic upwelling south of Africa.
Walker, N.D.
Deep Sea Research, v. 33, p. 1083-1106.
Sea surface temperature changes in continental shelf and deep ocean
environments south of Africa were monitored with calibrated and
atmospherically corrected thermal infrared satellite data from October
1983 to April 1984. The Agulhas Current played a dominant role in sea
surface warming of southest Atlantic Ocean water into the southeastern
Atlantic Ocean waters between October and January. Westward penetration of
Agulhas Current surface water into the southeast Atlantic Ocean was
greatest in April 1984 in association with higer than normal atmospheric
sea level pressure south of the continent. Positive surface temperature
anomalies of at least 4°C occurred west of 20°E as a result of this
intrusion. Simultanesouly, large-scale upwelling was observed over the
Agulhas Bank. The evolution, spatial characteristics and persistence of
abnormal upwelling events were assessed with satellite data, coastal
temperatures and wind measurements in comparison with climatological
means. The cool anomalies detected were primarily attributed to an
abnormal prevalence of easterly winds over the Agulhas Bank early in 1984.
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