Projections of hydrological changes and riverflow extremes using TerM land surface model in the Limpopo River Basin, South Africa
Open Access
- 15 September 2026
- journal article
- research article
- Published by Springer Nature in Theoretical and Applied Climatology
- Vol. 157 (10) , 654
Abstract
Increasingly frequent hydroclimatic extremes in South Africa necessitate a robust understanding of how changing climate drivers will influence regional water balance. This study evaluates the impacts of climate change on hydrological extremes within the Limpopo River Basin, a region historically vulnerable to catastrophic flooding and prolonged droughts. The INM RAS-MSU (Terrestrial Model; TerM) Land Surface Model was used to project river flow from 2020 to 2100. The atmospheric forcing was derived from the CMIP6 ISIMIP database under the SSP1-2.6 and SSP5-8.5 scenarios. Projections for the near future (2020–2055) and far future (2065–2100) periods were compared against a 1979–2014 baseline, with high-flow events (floods) computed at the 95th percentile. Intra-annual streamflow patterns remain consistent with historical trends but are projected to peak by more than 50%, particularly under the high-emission (SSP5-8.5) scenario. Peak flow increase will likely occur during the austral summer (January-February), while a pronounced decrease is projected during spring (September-November). Despite an increase in pronounced peaks in rainfall, evaporation, and runoff in May, the basin exhibits a statistically insignificant decreasing trend in these variables and annual streamflow between 2020 and 2100. This suggests a shift towards a more volatile regime, with intensified high-flow extremes in January and February punctuated by increasing dry conditions in March and September. Climate change is expected to intensify hydroclimatic extremes in northeastern South Africa, where austral summer rainfall variability is strongly influenced by tropical cyclones, the El Niño–Southern Oscillation (ENSO), and convective rainfall. The findings provide an evidence base for strengthening climate adaptation policies and measures to reduce the impacts of hydroclimatic extremes in northeastern South Africa.Keywords
Funding Information
- University of Limpopo
This publication has 53 references indexed in Scilit:
- Projections of extreme rainfall in South Africa using CMIP6 ISIMIP modelsClimate Dynamics, 2026
- Evaluating sunshine hour approximation for biometeorological indicesTheoretical and Applied Climatology, 2024
- Projections of Future Climate Change in Southern Africa and the Potential for Regional Tipping Points2024
- Performance evaluation of CMIP6 HighResMIP models in simulating precipitation over MadagascarInternational Journal of Climatology, 2023
- Projections of future fire risk under climate change over the South African savannaStochastic Environmental Research and Risk Assessment, 2023
- Noncoding RNAs and the borders of heterochromatinWIREs RNA, 2014
- Trends in extreme temperature indices in South Africa: 1962–2009International Journal of Climatology, 2012
- Dynamics of the Conformal‐Cubic Atmospheric Model projected climate‐change signal over southern AfricaInternational Journal of Climatology, 2008
- Temperature trends in South Africa: 1960–2003International Journal of Climatology, 2004
- URBAN INFLUENCES ON SOUTH AFRICAN TEMPERATURE TRENDSInternational Journal of Climatology, 1996