| dc.description.abstract | For rainfall-runoff modeling, precise rainfall measurements are required to examine the 
geographical and temporal patterns of rainfall at various scales. In many impoverished 
nations, such as Ethiopia, accurate and reliable rainfall monitoring is scarce. The Climate 
Hazards Group Infrared Precipitation with Stations (CHIRPS) and Precipitation 
Estimation from Remotely Sensed Information using Artificial Neural Networks-Climate 
Data Record (PRESIANN_CDR) satellite rainfall products for stream flow simulation are 
evaluated in this study at daily temporal and 0.05°×0.05° and 0.04°×0.04° spatial 
resolutions, respectively and simulated by HEC-HMS model. The Soil Conservation 
Service_Curve number, SCS_Unit Hydrograph, and Muskingum methods were utilized for 
loss, transformation, and routing computations, respectively, at the stated period and one day time step. The model was calibrated over fifteen years and the daily rainfall readings 
were verified during five years. The performance of HEC-HMS model and satellite rainfall 
was assessed using a coefficient of determination (R2
), Net-Sutcliffe Efficiency (NSE), Root 
Mean Square Error (RMSE), and Percent of BIAS. The model Calibration and Validation 
results were described here (R2 =0.81, NSE =0.84, RMSE = 0.5, PBIAS = +30.10) and 
(R
2=0.79, NSE = 0.82, RMSE = 0.4, PBIAS = +28.72) throughout the periods, 
respectively. Satellite rainfall products could be useful inputs for modeling in areas where 
field data is lacking for a variety of hydrological applications. The results revealed that 
the observed and simulated hydrographs were almost identical. The HEC-HMS model 
accurately predicted catchment runoff for both satellite rainfall products according to the 
findings. As a consequence, Neshi discharge was successfully simulated for the time period 
studied and the results suggested that the utilization of satellite rainfall data was 
appropriate or solve the problem of data scarcity and the model was adequate for 
hydrological simulations in the Neshi Watershed. | en_US |