Abstract:
ainfall during kiremt season is essential for Ethiopian agricultural operations. Improving sub
seasonal to seasonal rainfall forecasting is important to understand the distribution, frequency,
and intensity of rainfall in the country. This study was designed to enhance the current sub
seasonal to seasonal rainfall forecast by characterizing rainfall, evaluating the European Centre
for Medium-Range Weather Forecasts ERA5 performance, and applying multiple linear
regressions (MLR) and the nonlinear autoregressive network with exogenous inputs (NARX)
model. Daily gridded rainfall data recorded over 184 station points was analyzed to identify
rainfall onset, cessation, and length of growing periods. On the other hand, monthly gridded
rainfall and four predictors (SST3.4, ERA5 total precipitation, wind at 850 and 200 mb level)
covering the period of 1990 to 2020 were used to improve sub-seasonal to seasonal rainfall
forecasting and for model evaluation. The model's performance was evaluated using RMSE,
MAE, PBIAS, NSE, and R2. The result of this study indicates that the mean kiremt rainfall onset
begins southwestern early and progressively spreads across the country's central, western, and
northeast. This study generally finds that earlier onset dates for regions northeast, Central, and
east, northwest has a later average onset in the current study, while southwest is similar but ends
earlier. South highlands show a later start but an earlier end in the current study, whereas the
southern has an earlier start with a shorter duration. Northeast, northwest, southwest, east,
south highlands and south regions, consistently shows a later rainfall cessation. The
standardized Kiremt rainfall anomaly results show that the majority of the country was under
dry conditions during El Ni̱o years and wet during La Ni̱a years. The gridded data and the
ERA5 model's output from the ECMWF ERA5 reanalysis demonstrated a strong correlation, but
the model's underestimating rainfall value at both seasonal and sub-seasonal levels compared to
the actual across Ethiopia. The R2 results are 0.87 and 0.86 for the MLR and NARX models,
respectively, which indicate that the MLR model is slightly better suited to the observed data.
This study found that both MLR and NARX models demonstrate outstanding skill for rainfall
prediction for both seasonal and sub-seasonal levels of Kiremt seasons. The NARX model shows
strong results in capturing the rainfall patterns in Ethiopia, particularly during wet seasons, and
can provide valuable insights for understanding and predicting Kiremt rainfall in the country.
The MLR and NARX models�۪ performance varies across different stations and periods. These
results highlight the importance of considering different models and their strengths and
weaknesses when estimating kiremt month levels in specific locations. The results of this study
will improve early warning systems over Ethiopia in the fields of agriculture, hydrology, and
other related fields.