Impacts of combined and separate land cover and climate changes on hydrologic responses of Dhidhessa River basin, Ethiopia

被引:8
|
作者
Wedajo, Gizachew Kabite [1 ,2 ]
Muleta, Misgana Kebede [3 ]
Awoke, Berhan Gessesse [2 ,4 ]
机构
[1] Wollega Univ, Dept Earth Sci, POB 395, Nekemte, Ethiopia
[2] Ethiopia Space Sci Technol Inst, Entoto Observ Res Ctr, Dept Remote Sensing Res & Dev, POB 33679, Addis Ababa, Ethiopia
[3] Calif Polytech State Univ San Luis Obispo, Dept Civil & Environm Engn, San Luis Obispo, CA USA
[4] Kotebe Metropolitan Univ, Dept Geog & Environm Studies, Addis Ababa, Ethiopia
关键词
Hydrological responses; Dhidhessa River basin; land cover change; climate change impact; CHANGE SCENARIOS; WATER-RESOURCES; HEIHE RIVER; SWAT MODEL; USE/LAND COVER; NILE BASIN; STREAMFLOW; SIMULATION; CATCHMENT; QUALITY;
D O I
10.1080/15715124.2022.2101464
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
The combined effects of climate and land cover changes influence hydrologic responses of a basin in an offsetting or synergistic manner depending on the nature and severity of the changes. As such, estimating the impacts of these environmental changes on hydrologic responses is crucial for planning water resources management. However, such a comprehensive study is missing in most basins of Ethiopia, particularly in the Dhidhessa River basin (DRB). The aim of this study is, therefore, to quantify the combined and separate impacts of land cover and climate changes on multiple hydrologic variables for the DRB. The Calibrated Soil and Water Analysis Tool (SWAT) model and statistical techniques were integrated for this study. Quantifying the separate and combined effects of land cover and climate changes on multiple hydrologic responses at a local scale, and determining the relative contribution of the changes are the strength of this study. The result indicated better performance of the SWAT model in simulating water balance components for the DRB. Significant changes in hydrologic responses were observed in response to the land cover changes, and the increasing trends of temperature and rainfall observed during the last 30 years in DRB. The result showed increasing actual evapotranspiration (AET), streamflow, and surface runoff while decreasing groundwater recharge. Surface runoff was more affected by land cover change than by climate change, whereas streamflow and AET were more affected by climate change than land cover change during the last 30 years in the basin. The combined effects of land cover and climate changes played an offsetting effect on groundwater recharge and AET. Overall, the simulated hydrologic responses will have negative effects on water resource availability and agricultural production in the basin and the surroundings. Therefore, implementing integrated watershed management strategies, such as soil and water conservation and afforestation, could minimize the negative impact.
引用
收藏
页码:57 / 70
页数:14
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