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Analysis and Downscaling of Precipitation over East Africa and Djibouti: Observed Data, GCM-CMIP6, and CORDEX

This study provides a multi-scale comparison of simulated and observed precipitation. Global simulations from the CanESM5 model (CMIP6, 282 km) are contrasted with results obtained through stochastic downscaling at 3.5 km using CSTools. Observed rainfall for 1981 is spatially interpolated using Inverse Distance Weighting (IDW).

In addition, climate projections from the EC-Earth3-Veg model (CMIP6) under the SSP585 scenario are analyzed for the period 2021–2040, focusing on both the Republic of Djibouti and the wider East Africa region. Finally, downscaled daily precipitation from CORDEX (1981–1985) is generated using Nearest Neighbor and Bilinear interpolation, allowing an assessment of the sensitivity of results to methodological choices.


Figure 1. CMIP6 GCM CanESM5 precipitation for 1981 (spatial resolution: 282 km).


Figure 2. CMIP6 GCM CanESM5 precipitation for 1981 downscaled to 3.5 km using stochastic methods with CSTools.



Figure 3. Spatial distribution of observed rainfall in 1981 using Inverse Distance Weighting (IDW) interpolation




Figure 4. Projected total monthly precipitation (mm) from the EC-Earth3-Veg model (GCM-CMIP6), based on the ssp585 scenario Over the Republic of Djibouti during 2021-2040.



Figure 5. Projected total monthly precipitation (mm) from the EC-Earth3-Veg model (GCM-CMIP6), based on the ssp585 scenario Over the Eastern of Africa during 2021-2040.


Figure 6. Downscaled daily precipitation from CORDEX (1981–1985) using (a) Nearest Neighbor interpolation, (b) Bilinear interpolation, and (c) original CORDEX data for comparison


Abdi-Basid ADAN, 2023






The Abdi-Basid Courses Institute