| dc.description.abstract |
Studies of Hydro-climatic time series analysis and modeling are very crucial for planning
and management, and utilization of water resources of the Upper Awash River basin,
Ethiopia. This study aimed to evaluate hydroclimatic time series data and its modeling to
assess the impact of climate change on streamflow in the Upper Awash River basin. The
water balance components can be affected by climate change and need to be evaluated
through analyzing the impacts climate change. The non-parametric Mann-Kendall trend
test were adopted to detect and analyze trends in monthly, seasonal, and annual hydro
climatic variables. The influence of climate change on stream flow was assessed using the
Seasonal Autoregressive Integrated Moving Average with exogenous variables
(SARIMAX) model and selected four GCMs namely CCCMA, CNRM, ICHEC-EC
EARTH, and MPI with RCP4.5 and RCP8.5 scenarios. The GCM outputs for the base
period (1976-2005), short-term (2021-2050), and long-term period (2051-2080) forced the
calibrated and validated SARIMAX model. The calibration result showed that R2 is 0.95
and NSE is 0.81 were used, while for validation, an R2 is 0.99 and an NSE is 0.82. The
results of all GCMs also indicated that in the short and long term, temperature and
evapotranspiration will be increased under both RCP4.5 and RCP8.5 scenarios. The
projected annual streamflow, and precipitation showed that in the short and long term,
streamflow, and precipitation will be decreased under both the RCP4.5 and RCP8.5
scenarios. The study results can clearly reflect the overall situation of Climate change
impact on streamflow under two climate scenarios, and provide basis for planning,
management, and sustainable of water resources in the future. |
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