The impacts of LULC and climate change scenarios on the hydrology and sediment yield of Rib watershed, Ethiopia

被引:9
|
作者
Tsegaye, Lewoye [1 ]
Bharti, Rishikesh [2 ]
机构
[1] Bahir Dar Univ, Dept Nat Resource Management, Bahir Dar, Ethiopia
[2] Indian Inst Technol Guwahati, Dept Civil Engn, Gauhati, India
关键词
Climate change; Dyna-CLUE; LULC change; RCP; Scenario; Surface runoff; BLUE-NILE BASIN; LAND-USE CHANGES; COVER CHANGE; RIVER-BASIN; ASSESSMENT-TOOL; ANNUAL CYCLE; MODELS; CATCHMENT; DYNAMICS; VARIABILITY;
D O I
10.1007/s10661-022-10391-3
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Watershed-scale hydrology and soil erosion are the main environmental components that are greatly affected by environmental perturbations such as climate and land use and land cover (LULC) changes. The purpose of this study is to assess the impacts of scenario-based LULC change and climate change on hydrology and sediment at the watershed scale in Rib watershed, Ethiopia, using the empirical land-use change model, dynamic conversion of land use and its effects (Dyna-CLUE), and soil and water assessment tool (SWAT). Regional climate model (RCM) with Special Report on Emission Scenarios (SRES) and Representative Concentration Pathway (RCP) outputs were bias-corrected and future climate from 2025 to 2099 was analyzed to assess climate changes. Analysis of the LULC change indicated that there has been a high increase in cultivated land at the expense of mixed forest and shrublands and a low and gradual increase in plantation and urban lands in the historical periods (1984-2016) and in the predictions (2016-2049). In general, the predicted climate change indicated that there will be a decrease in precipitation in all of the SRES and RCP scenarios except in the Bega (dry) season and an increase in temperature in all of the scenarios. The impact analysis indicated that there might be an increase in runoff, evapotranspiration (ET), sediment yield, and a decrease in lateral flow, groundwater flow, and water yield. The changing climate and LULC result in an increase in soil erosion and changes in surface and groundwater flow, which might have an impact on reducing crop yield, the main source of livelihood in the area. Therefore, short- and long-term watershed-scale resource management activities have to be designed and implemented to minimize erosion and increase groundwater recharge.
引用
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页数:35
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