Research Article

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

Figure 11

Same as Figure 9, but for OND season. (a) OND 200- hpa wind clim. (b) OND 200- hpa wind anomaly. (c) OND RF and 850-hpa wind clim. (d) OND RF and 850-hpa wind anomaly. (e) OND low-level divergence clim. (f) OND low-level divergence anomaly