The results of this study show that large-scale SST variability over many parts of the tropical oceans is critically important in explaining Ethiopian rainfall variability. On seasonal to annual time-scales, the tropical Atlantic and the Arabian Sea exert strong influence on Ethiopian rainfall, while SST variations over the equatorial Pacific and the Indian Ocean become important for the biennial and ENSO modes. The results further show strong correlations between model-predicted and observed monthly rainfall totals/standardized all-Ethiopian June-September rainfall anomalies. For monthly rainfall predictions based on orthogonalized global SST with at least 3-month lead-time, the correlation between observed and predicted rainfall totals is +0.90 for 10 independent verification years. Predictions of all-Ethiopian standardized June-September rainfall anomalies also are highly successful. Based on orthogonolized global March SST predictions, the correlation between observed and predicted standardized June-September rainfall anomalies is +0.88 for 10-year retroactive verification.
The fact that the models explain more than 77% of the total rainfall variability when tested on independent data makes the wavelet-based predictions dependable and usable. Supported by knowledge of the requirements of the user community and decision makers, such accurate forecasts of monthly rainfall totals and seasonal anomalies months in advance would greatly help in combating the damaging effects of recurring droughts and reducing the adverse socioeconomic impacts of rainfall variability in Ethiopia.
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