Relative and Combined Impacts of Climate and Land Use/Cover Change for the Streamflow Variability in the Baro River Basin (BRB)

被引:0
|
作者
Kassaye, Shimelash Molla [1 ,2 ]
Tadesse, Tsegaye [3 ]
Tegegne, Getachew [4 ,5 ]
Hordofa, Aster Tesfaye [6 ]
Malede, Demelash Ademe [7 ]
机构
[1] Addis Ababa Univ, Africa Ctr Excellence Water Management, Hydrol & Water Resources Management, POB 1176, Addis Ababa 1176, Ethiopia
[2] Mattu Univ, Dept Water Resources & Irrigat Engn, POB 318, Mattu, Ethiopia
[3] Univ Nebraska Lincoln, Natl Drought Mitigat Ctr, Sch Nat Resources, 815 Hardin Hall,3310 Holdrege St, Lincoln, NE 68583 USA
[4] Addis Ababa Sci & Technol Univ, Dept Civil Engn, POB 16417, Addis Ababa, Ethiopia
[5] Addis Ababa Sci & Technol Univ, Sustainable Energy Ctr Excellence, POB 16417, Addis Ababa, Ethiopia
[6] Arba Minch Univ, Arba Minch Water Technol Inst, POB 21, Arba Minch, Ethiopia
[7] Debre Markos Univ, Dept Nat Resource Management, POB 269, Debre Markos, Ethiopia
来源
EARTH | 2024年 / 5卷 / 02期
关键词
CMIP6; SWAT plus; Baro River Basin; climate scenarios; land use/cover scenarios; HYDROLOGY;
D O I
10.3390/earth5020008
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The interplay between climate and land use/cover significantly shapes streamflow characteristics within watersheds, with dominance varying based on geography and watershed attributes. This study quantifies the relative and combined impacts of land use/cover change (LULCC) and climate change (CC) on streamflow variability in the Baro River Basin (BRB) using the Soil and Water Assessment Tool Plus (SWAT+). The model was calibrated and validated with observed streamflow data from 1985 to 2014 and projected the future streamflow from 2041 to 2070 under two Shared Socio-Economic Pathway (i.e., SSP2-4.5 and SSP5-8.5) scenarios, based on the ensemble of four Coupled Model Intercomparison Project (CMIP6) models. The LULCC was analyzed through Google Earth Engine (GEE) and predicted for the future using the Land Change Modeler (LCM), revealing reductions in forest and wetlands, and increases in agriculture, grassland, and shrubland. Simulations show that the decrease in streamflow is attributed to LULCC, whereas an increase in flow is attributed to the impact of CC. The combined impact of LULCC and CC results in a net increase in streamflow by 9.6% and 19.9% under SSP2-4.5 and SSP5-8.5 scenarios, respectively, compared to the baseline period. Our findings indicate that climate change outweighs the impact of land use/cover (LULC) in the basin, emphasizing the importance of incorporating comprehensive water resources management and adaptation approaches to address the changing hydrological conditions.
引用
收藏
页码:149 / 168
页数:20
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