Abstract
Evidence is presented of a connection between sea surface temperature (SST) variability in the tropical southeast Atlantic Ocean off Angola and boreal summer rainfall over coastal West Africa. The strongest relationships exist between April–May SST in the Angola‐Benguela Frontal Zone area, May–June latent heat fluxes in this area, and July–August rainfall over the region 5°W–5°E, 5°N–10°N. Anomalously wet summers in this region are also characterised by a weaker African Easterly Jet, a stronger Tropical Easterly Jet and, in many cases, reduced rainfall further north over the Southern Sahel.
Full Text 
Sign-in/Register to access full text options
Sign-in/Register to access full text options 
Published version (
Free)
Free) 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a call
