Abstract
In this study, we assessed the impact of climate change (CC) on the water balance of the Lake Hawassa catchment (a sub-catchment of the Rift Valley basin) in southern Ethiopia. The CMhyd (Climate model data for hydrologic modeling) was used to correct biases in the Representative Concentration Pathway (RCP) scenarios under the Hadley Global Environment Model 2-Earth System (HadGEM2-ES) for the 2050s (2041–2070) and 2080s (2071–2100). The CC impact analysis performed by the Soil and Water Assessment Tool (SWAT) demonstrated very reliable performance during the calibration (NSE = 0.81, R2 = 0.61) and validation (NSE = 0.85, R2 = 0.88) periods. Projected precipitation (PPT) is expected to increase by 3.4% and 6.9% in the 2050s, and reduce by 1.5% and 0.2% in the 2080s, respectively for the RCP4.5 and RCP8.5, while, respectively, minimum and maximum temperatures (Tmin and Tmax) are expected to increase by 0.6 °C and 3.2 °C under RCP4.5 and by 1.6 °C and 3.8 °C under RCP8.5. By the end of 2100, the long-term water balance of Lake Hawassa catchment under RCP4.5 and RCP8.5 showed PPT increased by 7.1% and reduced by 11.6%, surface runoff increased by 8.8% and reduced by 16.2%, lateral discharge reduced by 40.5% and 49.8%, water yield reduced by 19% and 39.4%, evapotranspiration increased by 21.1% and 19.2%, and potential evapotranspiration increased by 76.1% and 76.7% respectively. These results indicate that the water balance of the catchment will be altered by CC. Therefore, constantly monitored and updated sustainable water resource management and development is required.
Highlights
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Climate change scenarios were reviewed and bias correction was carried out for HadGEM2-ES Climate Model data
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Future precipitation and temperature were projected and their trend was assessed
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SWAT model was calibrated and validated for the years 1991–2002
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The projected change in temperature and rainfall impacts the hydrologic responses
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Impact of future climate changes on seasonal and annual water balance was quantified
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Data Availability
The DEM data is freely available at http://earthexplorer.usgs.gov and the dynamically downscaled daily-based RCPs climate data for the historical and future periods are freely available from http://cordexesg.dmi.dk/esgf-web-fe/ CORDEX Africa database.
Abbreviations
- AR5:
-
Fifth Assessment Report
- CC:
-
Climate Change
- CMhyd:
-
Climate Model Data for Hydrologic Modeling
- CN:
-
Curve Number
- CORDEX:
-
Coordinated Regional Climate Downscaling Experiment
- DEM:
-
Digital Elevation Map
- ET:
-
Evapotranspiration
- FAO:
-
Food and Agricultural Organization
- GCM:
-
Global Climate Model
- GIS:
-
Geographic Information System
- HadCM3:
-
Hadley Centre Coupled Model3
- HadGEM2-ES:
-
Hadley Global Environment Model2-Earth System
- HRU:
-
Hydrologic Response Unit
- IPCC:
-
Inter governmental Panel on Climate change
- LuLc:
-
Land use lands cover change
- MAE:
-
Mean Absolute Error
- MoWIE:
-
Ministry of Water and Irrigation Engineering
- NMA:
-
National Meteorological agency
- NSE:
-
Nash-Sutcliffe efficiency
- PET:
-
Potential Evapotranspiration
- PPT:
-
Precipitation
- R2 :
-
Coefficient of determination
- RMA:
-
Regional Meteorological Agency
- RCM:
-
Regional Climate Model
- RCP:
-
Representative Concentration Pathway
- RE:
-
Relative Error
- RMSE:
-
Root Mean Square Error
- SUFI2:
-
Sequential Uncertainty Fitting Version 2
- SCS:
-
Soil Conservation System
- SWAT:
-
Soil and Water Assessment Tool
- SWAT CUP:
-
Soil and water assessment tool Calibration and Uncertainty program
- Tmin&Tmax:
-
Minimum and Maximum Temperature
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Acknowledgements
We would like to acknowledge the Regional Meteorological Agency (RMA) of Hawassa and the National Meteorological Agency (NMA) of Ethiopia for providing the hydrological and meteorological data. And, our thanks go to the Ministry of Water Irrigation and Electricity (MoWIE) for providing streamflow, LuLc, and Soil data.
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Alehu, B.A., Bitana, S.G. Assessment of Climate Change Impact on Water Balance of Lake Hawassa Catchment. Environ. Process. 10, 14 (2023). https://doi.org/10.1007/s40710-023-00626-x
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DOI: https://doi.org/10.1007/s40710-023-00626-x