Opposite Effects of ENSO on the Rainfall over the Northern and Equatorial Great Horn of Africa and Possible Causes

<div>Time series of (a) summer rainfall averaged in the JJAS region and (b) autumn rainfall averaged in the OND region. The horizontal red lines in each panel are the ±1 standard deviation.</div>

Advances in Meteorology

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Figure 4

Figure 4: Opposite Effects of ENSO on the Rainfall over the Northern and Equatorial Great Horn of Africa and Possible Causes 