https://www.preprints.org/manuscript/202603.0667

*Authors: *Herbert O. Misiani, Betty N. Barasa, Franklin Joseph Opijah,
Hussen S. Endris, Jully O. Ouma, Christopher Lennard

*12 March 2026*

*Abstract*
This study evaluates the potential of solar radiation management (SRM) to
mitigate projected increases in rainfall and flood risk across four major
urban centers in Eastern Africa. Flood dynamics under historical and future
climate conditions were simulated using the Rainfall–Runoff–Inundation
(RRI) model. Observed hydrological conditions were established using daily
precipitation from the Climate Hazards Group Infrared Precipitation with
Stations (CHIRPS), together with hydrological and topographic datasets.
Future flood projections and associated impacts were derived from climate
simulations produced by the Whole Atmosphere Community Climate Model
version 6 (WACCM6) and solar climate intervention experiments from the
Assessing Responses and Impacts of Solar climate intervention on the Earth
system with Stratospheric Aerosol Injection (ARISE-SAI) framework, both
forced by the Shared Socioeconomic Pathway SSP2-4.5. Model performance was
evaluated using the Nash–Sutcliffe efficiency (NSE), coefficient of
determination (R2), root mean square deviation (RMSD), and peak discharge
error (PDE). The RRI model reproduced observed river discharge with
reasonable skill, exhibiting lower RMSD and PDE values for the Ethiopian
catchment compared to those in Kenya and Tanzania. Results indicate that
SRM implemented through stratospheric aerosol injection (SAI) can reduce
peak inundation depths and the spatial extent of flooding in selected
flood-prone areas of Dar es Salaam and Addis Ababa. These reductions
correspond to a decrease in the projected exposure of populations and
critical infrastructure to flood hazards. While the findings suggest that
albedo-based solar geoengineering may moderate flood impacts in some
Eastern African cities, uncertainties remain, particularly in the
representation of convective rainfall processes and the reliance on a
single hydrological modeling framework in this study. Further research
using improved climate simulations and ensemble-based hydrological
approaches is recommended.

*Source: Preprints.org*

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