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Published study · First author · Basin futures

What a drier future could mean for water in the Ruzizi Basin

Climate projections do not provide a single forecast. They show a range of plausible futures. In the Ruzizi River Basin, those futures consistently point toward less rainfall, lower water yield, and a more demanding management problem.

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Maximum rainfall decline
−37.86%
Water-yield decline
−52.10%
Mid-century window
2040—2069
Late-century window
2070—2100

How to read these numbers: the two maximum declines above refer to the mid-century SSP5-8.5 case relative to the model’s historical baseline.

01Question

How does a change in climate travel through an entire river basin?

A decline in rainfall does not translate directly into the same percentage decline in usable water. Temperature, evapotranspiration, soils, groundwater, and the timing of rainfall all shape the basin response. This study asks how those interacting processes could change water availability in the transboundary Ruzizi Basin through the middle and end of the century.

02Method

Connecting global climate scenarios to basin hydrology

The study combines observed and satellite climate data with a multi-model ensemble of downscaled CMIP6 projections. The SWAT hydrological model translates those climate inputs into rainfall, evapotranspiration, runoff, lateral flow, water yield, and streamflow. Simulations compare a historical baseline with 2040–2069 and 2070–2100 under SSP2-4.5 and SSP5-8.5.

  • CHIRPS
  • CMIP6 · MME
  • SWAT / SWAT-CUP
  • SSP2-4.5 · SSP5-8.5

03 / Findings

From rainfall to river flow: a cascading response

01

The scenarios become consistently drier

Mean annual precipitation decreases across both scenarios and future periods. The largest reported reduction is 37.86% by mid-century under SSP5-8.5, relative to the historical baseline.

02

Water yield responds more strongly than rainfall

The projected mid-century reduction in annual water yield reaches 52.10% under SSP5-8.5. This larger hydrological response shows why rainfall change alone is an incomplete measure of future water availability.

03

The seasonal water balance also changes

The monthly analysis projects lower rainfall and water yield throughout the year, with changes in evapotranspiration and lateral flow. Management therefore needs to consider when water is available as well as the annual total.

04

Lower flows raise a transboundary management question

The paper reports lower projected discharge in the basin’s lower reaches. That matters for domestic and agricultural water, ecosystems, and hydropower, all of which depend on a river shared by the Democratic Republic of the Congo, Rwanda, and Burundi.

Read the projections

The monthly water balance under two climate pathways

Eight charts comparing monthly rainfall, water yield, actual evapotranspiration, and lateral flow in the Ruzizi watershed for historical conditions and SSP2-4.5 and SSP5-8.5 projections in 2040–2069 and 2070–2100.

The left column shows the mid-century period and the right column the late-century period. Each row compares the historical baseline with SSP2-4.5 and SSP5-8.5 for rainfall, water yield, actual evapotranspiration, and lateral flow. The recurring separation between historical and projected water yield is the central signal.

Figure 6, Ahana et al. (2024). Reproduced unchanged; file format converted and display size adjusted. CC BY 4.0 · Source paper

04 / Contribution

My role as first author

This first-author paper anchors my work on climate change and water management in the Ruzizi Basin. It brings climate projections and basin modelling together to translate a global climate question into locally relevant evidence for water-resource decisions.

05 / Interpretation

These are conditional futures, not predictions

The results depend on the selected climate models, emissions pathways, downscaling, observed data, and SWAT representation of the basin. They describe what the model produces under stated assumptions; they do not predict a particular year’s rainfall or guarantee that one pathway will occur. Future land use, water demand, infrastructure, and management decisions can also change the outcome.

Publication

Water · 2024

Ahana, B. S., Nguyen, B. Q., Posite, V. R., Abdelbaki, C. & Kantoush, S. A. (2024). Future Projection of Water Resources of Ruzizi River Basin: What Are the Challenges for Management Strategy? Water, 16(19), 2783.