Seasonality of South African rainfall: a note on its regional delimitation using spectral analysis

1973 ◽  
Vol 21 (2-3) ◽  
pp. 207-214 ◽  
Author(s):  
Cecil S. Keen ◽  
Peter D. Tyson
Keyword(s):  
Spectral Analysis ◽  
South African ◽  
African Rainfall

scholarly journals Passive Suppression of South African Rainfall by the Agulhas Current

2015 ◽  
Vol 19 (13) ◽  
pp. 1-14 ◽  
Author(s):  
Mark R. Jury
Keyword(s):  
South African ◽  
Negative Influence ◽  
Rainfall Anomaly ◽  
Positive Influence ◽  
Cloud Band ◽  
Agulhas Current ◽  
Vegetation Fraction ◽  
African Rainfall ◽  
South Indian ◽  
And Cluster Analysis

Abstract This study reconsiders the role of the Agulhas Current in South African climate variability. Here, the Agulhas Current is delimited by its anticyclonic looping flow and cluster analysis of detrended SST anomalies that lead to an area 28°–37°S, 18°–35°E, poleward of South Africa. Regression of detrended Agulhas SST with rainfall anomaly fields in the years 1950–2012 yields a surprising negative influence over the interior. In summer, the negative regression exhibits a northwest axis consistent with reduced cloud band activity. Positive influence is confined to the eastern escarpment in the September–November season when cutoff lows are prevalent. The overall negative influence of the Agulhas SST is confirmed by regression with the vegetation fraction and latent heat flux in the satellite era. Mechanisms of South African rainfall suppression were investigated. The Agulhas SST index is positively related to the multivariate ENSO index at the 1–3-month lead time. Hence, warm years in the Agulhas Current follow Pacific El Niño. Composite ocean analysis shows enhanced westerly winds offshore and a westward extension of warm salty water from the anticyclonic south Indian Ocean gyre. Composite atmospheric analysis exhibits moist uplifted air over the Agulhas Current folding into an equatorward circulation that sinks over the interior plateau. Because Agulhas SST partially follows ENSO, its suppression of interior rainfall is concluded to be passive.

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