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

<div>Spatial patterns of the first three EOF modes of summer rainfall over the GHA (left panels) and the corresponding principal components: PC1, PC2, and PC3 (right panels), respectively. Red box in left panels is the JJAS region.</div>

Advances in Meteorology

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Figure 5

Figure 5: Opposite Effects of ENSO on the Rainfall over the Northern and Equatorial Great Horn of Africa and Possible Causes 