Assessment of spatial and temporal distribution of surface water balance in a data-scarce African transboundary river basin

被引:10
|
作者
Gelebo, Ayano Hirbo [1 ]
Kasiviswanathan, K. S. [1 ,2 ]
Khare, Deepak [1 ]
Pingale, Santosh Murlidhar [3 ]
机构
[1] Indian Inst Technol, Dept Water Resources Dev & Management, Roorkee 247667, Uttar Pradesh, India
[2] Indian Inst Technol, Mehta Family Sch Data Sci & Artificial Intelligen, Roorkee, Uttar Pradesh, India
[3] Natl Inst Hydrol, Hydrol Invest Div, Roorkee, Uttar Pradesh, India
关键词
surface water balance; water deficit; model parameter sensitivity; WetSpass-M; Omo River basin; Ethiopia; RAINFALL-RUNOFF MODEL; GROUNDWATER RECHARGE; RESOURCES ASSESSMENT; UNCERTAINTY ANALYSIS; LOESS PLATEAU; CATCHMENT; EVAPOTRANSPIRATION; VARIABILITY; SENSITIVITY; WETSPASS;
D O I
10.1080/02626667.2022.2094268
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
Assessment of the spatial and temporal distribution of surface water balance (SWB) components for a river basin having complex topography with limited observed data is challenging. This paper focused on estimating the spatial-temporal variability of long-term average monthly, seasonal, and annual SWB components using the modified Water Energy Transfer between Soil, Plants, and Atmosphere in Steady State (WetSpass-M) physically based hydrological model in Ethiopia's data-scarce Omo River basin. Further, the model output was used for estimating the spatial variation of the average monthly crop water deficit. A sensitivity analysis was performed on the global and local parameters of the model for analysing the relative variation in the SWB components. It was found that actual evapotranspiration (AET) and interception are insensitive to average rainfall intensity while surface runoff is highly sensitive. The variation of SWB under different combinations of land-use/land cover (LU/LC) and soil type indicates that SWB types such as surface runoff, AET, and interception are influenced more by LU/LC than by soil type.
引用
收藏
页码:1561 / 1581
页数:21
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