Andreas Persson

Study region: The Limpopo River Basin (LRB) is a transboundary catchment in Southern Africa, shared by South Africa, Botswana, Zimbabwe, and Mozambique. The basin is increasingly affected by climate variability, land-use change, and rapid population growth, with the Chókwe floodplain in Mozambique representing a hotspot of socio-economic vulnerability to floods. Study focus: This study applies the HYPE hydrological model, driven by nine bias-corrected Regional Climate Models (RCMs), to project future high-flow extremes in the LRB under two emission scenarios (RCP 4.5 and RCP 8.5). To account for non-stationarity, flood frequency analysis was performed using the Gumbel distribution within two quasi-stationary time slices: mid-century (2030–2064) and late-century (2065–2099). Additional intensity–duration–frequency (IDF) analysis was used to evaluate changes in short-duration rainfall extremes. New hydrological insights for the region: By the late century, ensemble projections indicate that 50-year floods will increase by ∼84 % under RCP 4.5 and ∼106 % under RCP 8.5, while 100-year floods may rise by ∼116 % and ∼142 %, respectively, compared to the historical baseline (13,551 m³/s). IDF analyses indicate an intensification of short-duration rainfall, particularly under RCP 8.5. These results suggest that floods of historically rare magnitude may recur multiple times within a century, posing increasingly significant risks to infrastructure, agriculture, and settlements in the Lower Limpopo. The findings emphasise the need for adaptive flood management, updated design standards, and strengthened transboundary cooperation in the basin.