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

<div>The difference of SST (shaded in °C) and 850-hPa wind (streamline) in (a) JJAS between El Niño years and La Niña years, (b) OND between El Niño years and La Niña years, and (c) OND between pIOD years and nIOD years.</div>

Advances in Meteorology

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Figure 10

Figure 10: Opposite Effects of ENSO on the Rainfall over the Northern and Equatorial Great Horn of Africa and Possible Causes 